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"topographically" Definitions
  1. in a way that is connected with the physical features of an area of land, especially the position of its rivers, mountains, etc.
"topographically" Synonyms
environmentally geographically naturally structurally physically terrestrially geologically regionally territorially zonally

545 Sentences With "topographically"

How to use topographically in a sentence? Find typical usage patterns (collocations)/phrases/context for "topographically" and check conjugation/comparative form for "topographically". Mastering all the usages of "topographically" from sentence examples published by news publications.

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"It's on a high point in the city topographically, so it gives amazing views," Mr. Powell said.
The only physical process to drive weather, then, would be land breezes, sea breezes, and topographically-induced winds.
The previously drab beige appearance has been replaced with a map that is more topographically and ecologically accurate.
The north-eastern state of Assam is among the most ethnically, linguistically, religiously and topographically mixed bits of India.
The final section includes an example of Le Brun's landscape painting, a topographically fanciful depiction of a Swiss festival.
My stomach, which was now topographically comparable to a road in rural Liberia, was a badge of honor, they said.
Participants will slip on a spacesuit and helmet and effectively fly to Mars, where they can explore a topographically accurate landscape.
Things are not contained either at the Sifang Museum, itself a topographically intriguing structure that flirts with parallel and linear perspectives.
No, unexpectedly, the toughest part of the 7.5-mile Dipsea, a topographically schizophrenic romp that was first run in 1905, could be mental.
To get a bit more specific, topographically speaking, buildings can be cut to measure from styrofoam blocks, on a giant lathe in the basement.
Only five percent of the seafloor has been topographically imaged, which leaves 1003 percent of the entire planet (not counting land masses) relatively unknown.
Cromarty's pictorial structure reverses perspectival illusion — instead of the image receding into the picture plane, the topographically stacked cardboard causes the image to rush forward.
With the Baltic Sea as its backdrop, the archipelago ranges topographically from barren coastal cliffs to stunning white-sand beaches to forests and fertile farmland.
The unassuming park (aside from the open-air concrete pavilion, it appears architecturally and topographically boring) is one of T.Y.E.'s three Oak Cliff must-see's.
Once the hotel's complete, you'll be able to ski down five levels of the building's exterior, using a topographically suited path that leads to local ski trails at the foot.
Topographically speaking, there is an extensive network of trails into mountains and along flat areas, cities are committed to bike lane expansions, and there are races all year long, both amateur and professional. Gov.
The area studied was topographically flat, about 20 kilometers, or 12 miles, wide and seasonally covered by a relatively thin layer of carbon dioxide ice that's no more than 1.5 kilometers, or 0.9 miles, deep.
As far as I knew, Mr. Dart was neither a climate skeptic nor a denier, and yet he continued to acquire significant parcels of a country that was, topographically speaking, one of the most vulnerable on earth.
But ecologists Greta Dargie and Simon Lewis of the University of Leeds suspected that we might find peat if we looked for it, particularly in a wet, topographically-depressed region of the Congo's interior, known as the Cuvette Central.
It records a city that had not yet been topographically reshaped to make room for its explosive growth in the second half of the 19th century; today, very little of those waterways can be seen without intrepid exploration in sewer lines.
Initially conceived as a surveying laser technology for creating topographically maps of hard-to-reach areas — including the surface of the Moon in the Apollo 15 mission — LIDAR has become pivotal to self-driving cars because it turns out that pulses of light are great for measuring the distance of objects from one another.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable tables comprise the most topographically prominent mountain peaks of greater North America. Each of these 353 summits has at least of topographic prominence.
Mount Rose is the highest mountain in Washoe County, within the Carson Range of Nevada, United States. It ranks thirty-seventh among the most topographically prominent peaks in the state. It is also both the highest and most topographically prominent peak of the greater Sierra Nevada range within the state of Nevada, and the third most topographically prominent peak in the Sierra Nevada overall. It is located in the Mount Rose Wilderness of the Humboldt-Toiyabe National Forest.
Savo Island, a volcanic cone northwest of Guadalcanal, is a topographically significant island in the eastern region.
Grapevine Peak is the highest mountain in the Grapevine Mountains of Nye County in Nevada, United States. It is the fourth-most topographically prominent peak in Nye County and ranks seventeenth among the most topographically prominent peaks in Nevada. The peak is located within the boundaries of Death Valley National Park.
Bald Mountain is the highest mountain in the Pine Grove Hills of Lyon County in Nevada, United States. It is the most topographically prominent peak in Lyon County and ranks eighty-second among the most topographically prominent peaks in Nevada. The peak is located within the Humboldt-Toiyabe National Forest.
Star Peak is both the highest and most topographically prominent mountain in both the Humboldt Range and Pershing County in Nevada, United States. It is the sixth-most topographically prominent peak in Nevada. The peak is on public land administered by the Bureau of Land Management and has no access restrictions.
Topographically, Manhattan is relatively flat, except the immediate coastal region which consists of a stepper ridge leading to the beach.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 209 most topographically isolated mountain peaks of the United States of America (including its territories) with at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence.
Mount Siegel is the highest mountain in the Pine Nut Mountains of Douglas County in Nevada, United States. It is the most topographically prominent peak in Douglas County and ranks forty-sixth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.
Mount Augusta is the highest mountain in the Clan Alpine Mountains of Churchill County in Nevada, United States. It is the most topographically prominent peak in Churchill County and ranks nineteenth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.
Quinn Peak is the highest mountain in the Jackson Mountains of Humboldt County in Nevada, United States. It is the most topographically prominent peak in Humboldt County and ranks tenth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.
Mormon Peak is the highest mountain in the Mormon Mountains of Lincoln County in Nevada, United States. It is the most topographically prominent peak in Lincoln County and ranks twenty-fourth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.
The most topographically prominent mountain in Humboldt County is unofficially known as Dan Dobbins Peak and is in the remote Jackson Mountains.
It is also the most topographically prominent peak in the county and the second-most prominent peak in Nevada (after Mount Charleston).
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 65 ultra-prominent summits of the U.S. State of Alaska. Each of these peaks has at least of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 128 ultra-prominent summits of the United States of America. Each of these peaks has at least of topographic prominence.
Rockingham is topographically flat, has sandy soils and coastal vegetation. It has a northern aspect to Cockburn Sound, from Rockingham Beach and Palm Beach.
Portion of parish of Berringa, Bethanga gold field, county of Benambra / geologically and topographically surveyed by J.P.L Kenny, B. C. E Assistant Field Geologist, 1908.
Piper Peak is the highest mountain in the Silver Peak Range of Esmeralda County in Nevada, United States. It is the most topographically prominent peak in Esmeralda County and ranks twenty-third among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions. The summit was named after N. T. Piper.
Mount Tobin is the highest mountain in the Tobin Range of Pershing County in Nevada, United States. It is the second-most topographically prominent peak in Pershing County and ranks twelfth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions, though private property is located along the most popular route to the summit.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 200 most topographically prominent mountain peaks of the United States of America. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.All elevations in the 48 states of the contiguous United States include an elevation adjustment from the National Geodetic Vertical Datum of 1929 (NGVD 29) to the North American Vertical Datum of 1988 (NAVD 88).
Bashmachnikov, I., Loureiro, C.M. & Martins, A., 2013. Topographically induced circulation patterns and mixing over Condor seamount. Deep-Sea Research Part II: Topical Studies in Oceanography, 98, A: 38–51.
Virginia Peak is the highest mountain in the Pah Rah Range of Washoe County in Nevada, United States. It is the most topographically prominent peak in Washoe County and ranks thirty-sixth among the most topographically prominent peaks in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions. A National Weather Service NEXRAD doppler weather radar station is located on the summit.
Elvestad is host to the municipality administration and an Asylum-Seeker Centre. Topographically it is situated in a small valley that is around two kilometers wide at the widest point.
Neighboring Dolores Peak on the same drainage divide may be higher than Middle Peak. If this is the case, Dolores Peak would be the more topographically prominent of the two summits.
Dolores Peak may be higher than neighboring Middle Peak on the same drainage divide. If this is the case, Dolores Peak would be the more topographically prominent of the two summits.
By contrast the prominence of Wheeler Peak, at , is the twelfth largest in the contiguous United States. It is also the twelfth most topographically isolated summit in the contiguous United States.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 200 most topographically isolated mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Mount Grant is both the highest and most topographically prominent mountain in both the Wassuk Range and Mineral County in Nevada, United States. It ranks thirteenth among the most topographically prominent peaks in the state. The peak is located within the Hawthorne Army Depot, resulting in very limited public access. Mount Grant was named after Ulysses S. Grant (1822–1885), general of the Union during the American Civil War and afterward 18th President of the United States.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a susexxleast of topographic prominence. All summits in this article have at least 500 meters of topographic prominence.
Hiệp Hòa is topographically uneven, with hills and low mountains in some communes in the north, the Red River Delta in the east and generally sloped from the northwest to the southeast.
Since the end of the Miocene the area of the Gulf of Suez rift has begun to experience post-rift thermal subsidence accompanied by flooding of the topographically lowest parts of the rift.
Gilbert Munger (April 14, 1837 – January 27, 1903) was a late 19th-century American landscape painter whose romantic yet topographically accurate landscapes helped to introduce the newly opened West to the American public.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table lists the 113 mountain peaks of the United States with at least of topographic isolation and at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 302 mountain peaks of the United States with at least of topographic elevation and at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 104 mountain peaks of the United States with at least of topographic elevation and at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Otherwise known as Mount McKinley, it is the third-most topographically prominent and third-most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 200 highest mountain peaks of the United States with at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 23 mountain peaks of the U.S. State of Alaska with at least of topographic elevation and at least of topographic prominence. Topographic elevation is the vertical distance above the reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface.
There are 22 Marilyns and 28 Hewitts in the Yorkshire Dales National Park. Topographically, the boundaries of the Yorkshire Dales trace the flow of streams from the lowest points between it and the neighbouring regions of the Lake District, North Pennines, Forest of Bowland, South Pennines and North York Moors. Hills are grouped as topographically as possible, according to their 'parent Marilyn'. The parent Marilyn of hill A can be found by dividing the nearby area into territories, by tracing the runoff from the key col of each Marilyn.
Diamond Peak is both the highest and most topographically prominent mountain in both the Diamond Mountains and Eureka County, in Nevada, United States. It ranks thirty-ninth among the most topographically prominent peaks in the state. The peak is located on the border of Eureka County and White Pine County, about 12 miles northeast of the small town of Eureka, between the south end of Diamond Valley and the central portion of Newark Valley. It is on public land administered by the Bureau of Land Management and thus has no access restrictions.
The Großer Widderstein (or just Widderstein) is a mountain, , in the west Austrian state of Vorarlberg. Topographically it belongs to the Allgäu Alps. It is the highest peak in the subgroup of the Southeastern Walsertal Mountains (Südöstliche Walsertaler Berge).
Spruce Mountain is a mountain in Elko County, Nevada, United States. It was named from the spruce timber near the summit. Spruce Mountain ranks twenty- fifth among the most topographically prominent peaks in the state. The summit is at .
According to the U.S. Census Bureau, the county has a total area of , of which is land and (0.5%) is water. The tallest and most topographically prominent mountain in Pershing County is Star Peak at 9,840 ft (3,000 m).
The Goose Creek Mountains are a mountain range in Box Elder County, Utah. They are also partly in Elko County, Nevada. It is the least topographically prominent of Utah's peaks with more than 609.6 ft (2000 ft) of prominence.
The prints and drawings collection is similarly arranged to the photograph collection, with a greater focus on the inner London areas. It is also arranged both topographically and by subject. Most of the prints and drawings date from the 18th and 19th centuries.
Highland continents—or terrae—are areas of topographically unstable terrain, with high peaks and valleys. They resemble highlands on Earth, but the term is applied to much larger areas on other planets. They can be found on Venus, Mercury, Mars and the Moon.
The creek passes through stone and concrete culverts when flowing under Main Avenue. Numerous stream segments have braided flows or channel loss. The creek flows through 21 pipes, whose diameters range from . Keyser Creek is topographically very similar to the nearby Saint Johns Creek.
Bowdoin is situated on the north side of Beacon Hill, and runs north to south. It is primarily a residential street. Topographically, Bowdoin Street is a hill from Cambridge Street at the bottom to its north, and Beacon Street at the top to its south.
Aerial view (1966) The locality Winterberg is the topographically highest township of Lindau. There some traditional farmers in the village, and in the early 1930s the first one- family houses were built. Until today the building activity has been continued on a moderate speed.
3:1 (Spring/Summer 1991), p. 10-33, 16. The 2000 and 2100 blocks of P Street NW in 2012 P Street NW was important both commercially and topographically. The P Street ford marked the farthest point at which ocean-going ships could travel up Rock Creek.
The community lies in the Spessart range of hills. It is located in the Aschaffenburg district in the Regierungsbezirk of Lower Franconia (Unterfranken). Topographically, the town is located at an elevation of around 350 m in the valley of the Weibersbach, which is a side valley of the Hafenlohrtal.
Castello di Mussomeli in alt=Musomeli Burg Chiramonte.jpg A rock castle () is a type of medieval castle that directly incorporates natural rock outcrops into its defences to such an extent that the rock formations define the structure of the castle. Topographically, rock castles are classified as hill castles.
This process can redistribute large loads from an elevated region to a topographically lower area as well – thus promoting an isostatic response in the region of denudation (which can cause local bedrock uplift). The timing, magnitude, and rate of denudation can be estimated by geologists using pressure-temperature studies.
Denali in Alaska is the highest mountain peak of North America. Denali is the third-most topographically prominent and third-most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 200 highest mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 11 mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 401 mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 124 mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. The following sortable table comprises the 230 mountain peaks of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Denali in Alaska is the highest mountain peak of North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. This article comprises four sortable tables of mountain summits of greater North AmericaThis article defines greater North America as the portion of the continental landmass of the Americas extending westward and northward from the Isthmus of Panama plus the ocean islands surrounding that landmass. This article defines the ocean islands of greater North America to include the coastal islands of North America, the islands of the Caribbean Sea, the Lucayan Archipelago, the islands of Greenland (Kalaallit Nunaat), the islands of Canada, and the islands of Alaska.
Prior to 2000, Gorontalo province was part of North Sulawesi province which lies on the eastern border. The western border of the province is Central Sulawesi province. Topographically, the province is relatively low (0–40o), with the elevation ranging between 0– above sea level. Its coastline length is more than .
The system of building number generally follows the British pattern. With many streets (e.g., Grafton Street, Baggot Street Lower), numbers proceed sequentially up one side of the street to its terminus and then continue down the other side. The numbers usually begin in topographically lower areas and proceed upward, i.e.
Holderness from space. Holderness is an area of the East Riding of Yorkshire, on the east coast of England. An area of rich agricultural land, Holderness was marshland until it was drained in the Middle Ages. Topographically, Holderness has more in common with the Netherlands than with other parts of Yorkshire.
After the inspection of several sites, it was discovered that Yokosuka topographically, if on a smaller scale, resembled the port of Toulon, France. It was decided to establish the shipyard here. It would be called the "Yokosuka Iron Works". In 1871, the name was changed to the "Yokosuka Navy Yard".
While not of exceptional height for New Mexico mountains, South Baldy is surrounded by low terrain, and hence is a highly visible landmark and the sixth most topographically prominent peak in the state. The eastern view from the summit of South Baldy. The western view from the summit of South Baldy.
Cepos de ancla romanos, en Prehistoria y Arqueologia de las Islas Baleares. VI Simposium de Prehistoria Peninsular, 1974, pp. 452. Intact Roman glass cup from Sanitja. Type Vessberg C. I/III In 1994 an underwater visual inspection was carried out, where some materials were identified and topographically recorded, including isolated materials (anchor sites).
The coniferous vegetation is represented by two gymnosperm families, Cupressaceae (Diselma archeri, Athrotaxis cupressoides, A. selaginoides) and Podocarpaceae (Michrocachrys tetragona, Microstrobos niphophilus, Podocarpus lawrencei). This vegetation type has a patchy distribution in areas topographically protected from fire. This vegetation would likely be the climax vegetation of the region in the absence of fire.
Topographically the gap is a pass (small cleft) caused by a tectonic plate shift (according to Roger Latham), between east and west hill ranges. A tributary of the River Nene rises at Watford and flows east to the Wash, whereas at Kilsby a tributary of the River Leam rises and flows west.
Bagh is located 80 kilometres from Muzaffarabad, the capital city of Azad Kashmir. It is 160 kilometres from Islamabad, the capital of Pakistan.Bagh, Pakistani Tourism Topographically, the district is quite mountainous with lush green pine forests on the mountain slopes leading into the valleys. The altitude of Bagh Valley is 3405 feet (1038m).
"Topographically speaking, the island merits little study, but it is the location of one of the Abarat's most extraordinary buildings: the Repository of Remembrance", which is the Abarat's most famous museum. "The toys of emperors, the rag dolls of queens", and other now useless but historically and sentimentally valuable objects are kept here.
A nickname given to Tech's academic administration and historic district. Topographically, Tech's first administrative buildings were built on an actual hill in Atlanta. As campus expanded onto surrounding lower terrain, the Hill became a much more prominent sight on campus. The term now is typically used in derision when referring to the administration.
Two potential transportation mechanisms for the metal-bearing ore fluid have been proposed. The first involves compaction of sediments in basins with rapid sedimentation. Mineralizing fluids within the basin become trapped within discrete, over-pressured aquifers and escape episodically and rapidly. The second fluid transportation mechanism is topographically-driven gravitational fluid flow.
Map of Bagh district Topographically, the entire Bagh district is a mountainous area, generally sloping from northeast to south-west. The area falls in the lesser Himalayas zone. The main range in the district is Pir-Panjal. The Haji-Pir Pass is situated at the height of 3421 meters above sea level.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
Mount Moriah is a mountain in the northern Snake Range of eastern White Pine County, Nevada, United States. It is the fifth-highest mountain in the state, and also ranks as the ninth-most topographically prominent peak in the state. It is located in the Mount Moriah Wilderness administered by the Humboldt- Toiyabe National Forest.
70, Sishu Sahitya Sansad The Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
The volcano is high and is topographically prominent because it rises from lowland areas near sea level in the south of the Big River. Based on radiocarbon dating the caldera-forming eruption occurred about 5800 years before present. During this eruption at least were covered in a dacitic ignimbrite. Map showing volcanoes of Alaska.
Hayford Peak, elevation , is the highest mountain in the Sheep Range of Clark County, Nevada, United States. It is the seventh-most topographically prominent peak in the state. The nearest taller mountain is Mount Charleston, to the southwest. In the winter months, there is snow on the peak, which usually lasts until early spring.
Users can browse and search topographically-shaded street maps for many cities worldwide. Maps include certain points of interest built in, such as metro stations, stadiums, hospitals, and other facilities. It is also possible to browse public user- created points of interest. Searches can cover public collections, businesses or types of business, locations, or people.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
Its lava field at Roiho has been dated at between 110,000 and 150,000 years old. Terevaka is an easy walk up on a trail that starts next to the moai at Ahu Akivi, by foot or horse. It is often very windy at the top. Terevaka is the 12th most topographically isolated summit on Earth.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north- western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
Topographically, Alamata is divided into western highland and eastern lowland. The western part (Tsetsera and Merewa) is categorized under the northern highlands of Ethiopia, having an altitude range of . It is characterized by steep slopes, gorges and undulating terrain having scattered flat lands used for grazing livestock and farming. It covers 25% of the woreda.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
Crowders Mountain State Park is the largest natural heritage site in the county. It covers over of topographically, botanically, and zoologically diverse land. Six natural plant communities are found in the park, and the area supports a diversity of wildlife species. Some animals documented in the park have not been documented elsewhere in the county.
70, Sishu Sahitya SansadThe Tehatta subdivision, presented in the map alongside, is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision. The other important rivers are Mathabhanga and Bhairab. The eastern portion forms the boundary with Bangladesh.
Topographically, the Gomati district is marked by lush green and fertile Gomati valleys. The towering Debtamura hill range which straddles Udaipur and Amarpur subdivisions of the district with its exquisite sculptural works carved on panels of the hills. There are 173 villages in this district. The whole district is served by 16 police stations.
The whole region is hilly and mountainous topographically, but every part of the valley is easily accessible. The Karakoram mountain range covers the whole region, of which Rakaposhi is one part. Of the total area of Nagar valley, 90% is above 3,000 meters above sea level and 30% is 5,000 meters above sea level.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The plains spread southwards from the head of the delta. The Tehatta subdivision is topographically part of the Nadia Plain North. The Jalangi River forms the district/ subdivision border in the north-western part and then flows through the subdivision.
A precipitationshed is the upwind ocean and land surface that contributes evaporation to a given, downwind location's precipitation. In much the same way that a watershed is defined by a topographically explicit area that provides surface runoff, the precipitationshed is a statistically defined area within which evaporation, traveling via moisture recycling, provides precipitation for a specific point.
This is a list of mountains of the Swiss canton of Glarus. Glarus is a very mountainous canton and lies entirely within the Alps. It is also one of the five cantons having summits above 3,600 metres. Topographically, the most important summit of the canton is that of the Tödi (most elevated, most prominent and most isolated).
This is a list of mountains of the Swiss canton of Uri. Uri is a very mountainous canton and lies entirely within the Alps. It is also one of the five cantons having summits above 3,600 metres. Topographically, the most important summit of the canton is that of the Dammastock (most elevated, most prominent and most isolated).
The reticulotegmental nucleus also receives efferent axons from the cerebellum. This nucleus is known for its large number of multipolar cells and its particularly reticular structure. The reticulotegmental nucleus is topographically related to pontine nuclei (non-reticular), being just dorsal to them. The reticulotegmental nucleus has been known to mediate eye movements, otherwise known as saccadic movement.
This area was chosen for this purpose as it is one of the only areas to topographically satisfy the pertinent legal requirements. The area is also well used by visiting school children on environmental education trips as it has been installed with several large wood carvings that aid environmental interpretation. The area is still being developed for both purposes.
This is the most attractive molasse mountain range sculpted in the entire Alps. The lower mountains further north also form small chains. The central part of the Tannheim group is made of Wetterstein limestone, a reef limestone. This accounts for the isolated location of these mountains which are not topographically connected to the main chain of the Allgäu Alps.
The ' ('messenger poem') genre is one of the best defined in Indian literature. There are about 55 messenger poems in Sanskrit, plus others written in vernacular tongues. These span India chronologically, topographically and ideologically: there are Muslim and Christian messenger poems, and poets are still composing these poems today. Each follows Kalidasa's Meghaduta to a greater or lesser extent.
Brahmanbaria () is a district in eastern Bangladesh located in the Chittagong Division. Geographically, it is mostly farmland and is topographically part of the Gangetic Plain. It is bounded by the districts of Kishoreganj and Habiganj to the north, Narsingdi District and Narayanganj to the west, Comilla to the south, and the Indian state of Tripura to its east.
Kilimanjaro is the 4th most topographically prominent peak on Earth. The first people known to have reached the summit were Hans Meyer and Ludwig Purtscheller, in 1889. It is part of Kilimanjaro National Park and is a major climbing destination. Because of its shrinking glaciers and disappearing ice fields, it has been the subject of many scientific studies.
Pilot Peak (Shoshoni: Waahkai) is the highest mountain in the Pilot Range in extreme eastern Elko County, Nevada, United States. It is the most topographically prominent peak in Elko County and the fourth-most prominent peak in Nevada. The peak is on public land administered by the Bureau of Land Management and thus has no access restrictions.
This is a list of the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Central Asia. The list is divided topographically rather than politically. There are 75 in total; 21 in the Pamirs, 1 in the Karakum, 5 in the Alays, 24 in the Tian Shan and 24 in the Altai and Mongolia.
Chapter 28, Observations and Impressions from Lunar Orbit. PDF file The name derives from the roughly semicircular shape of the border of the feature, resembling a helmet. The feature is topographically higher and of a higher albedo than the surrounding mare lava plain. Two mountains within The Helmet are informally named Herigonius Eta (η) and Herigonius Pi (π).
The dunes were fortified and used for exercises in the Second World War. There is a roughly square MoD danger area and base inland of the east of the area. The dunes resemble topographically those seen in parts of Normandy and challenging desert terrain. Similar training facilities exist at Braunton in North Devon, in Scotland and in Pembrokeshire.
It was probably completed in 1432 and 1433, with later supplements and corrections. The properties of the archdiocese included several thousand farms. The records in the land register are arranged topographically by counties within the diocese. The cadastre is regarded as an important primary historical source, both for historical economic research, and for research of place names.
Topographically, Bellevue is higher in elevation than its neighboring cities. When the Ohio River would rise, homes in Dayton and Newport would flood while homes in Bellevue (with the exception of homes in proximity to the riverbank) remained safe from rising water. For this reason, Bellevue is not protected by a levee, whereas Dayton and Newport are.
Kerinci people (; Jawi: كرينچي) is one of the ethnic group in Kerinci Regency, Sungai Penuh, Merangin Regency, West Sumatera, Malaysia, and other districts.Ensiklopedia Suku bangsa It covers an area of 4,200 km² with a population of 300,000. Topographically Kerinci Regency owns hilly terrain in a row of the Bukit Barisan Range with the highest peak of Mount Kerinci.
The western Troutbeck side is steep and smooth, except for the ravine of Blue Gill. This rends the fellside from top to bottom and is a feeder of Hagg Gill. The Kentmere flank is rougher and falls in fans of scree to the River Kent, just above Kentmere Reservoir. Topographically, Froswick has one feature which Ill Bell lacks - a subsidiary ridge.
Topographically Pothuwila village is based on a plain area with the exception of the surrounding rock outcrops. The northern part of the town is slightly higher than the south. The Pothuwila Lake is the primary geographical feature of Pothuwila. The region comprising the Pothuwila village is located well above the sea level compared to the coastal areas of Sri Lanka.
Montfort Castle from southwest, stretching down a spur Topographically, a spur is a narrow ridge projecting from a larger hill. Built on this defensible feature, Montfort is a spur castle. The defences are concentrated at the most vulnerable eastern side where the spur joins the hill. On that side there are two ditches in front of a large D-shaped tower.
This is a list of mountains of the Swiss canton of Schwyz. Schwyz is a very mountainous canton and lies almost entirely within the Alps. It is also one of the 15 cantons having summits above 2,000 metres. Topographically, the two most important summits of the canton are those of the Bös Fulen (most elevated) and the Rigi (most prominent and isolated).
Topographically Kurunegala town is based on a plain area with the exception of the surrounding rock outcrops. The northern part of the town is slightly higher than the south. Kurunegala Lake is the primary geographical feature of Kurunegala and adorns the town. The region comprising the Kurunegala town is well above the sea level compared to the coastal areas of Sri Lanka.
Areas of upwelling in red The major upwellings in the ocean are associated with the divergence of currents that bring deeper, colder, nutrient rich waters to the surface. There are at least five types of upwelling: coastal upwelling, large-scale wind- driven upwelling in the ocean interior, upwelling associated with eddies, topographically-associated upwelling, and broad-diffusive upwelling in the ocean interior.
In the late 19th century, John Langley discovered that the superior cervical ganglion is topographically organized. When certain areas of the superior cervical ganglion were stimulated, a reflex occurred in specified regions of the head. His findings showed that preganglionic neurons innervate specific postganglionic neurons. In his further studies of the superior cervical ganglion, Langley discovered that the superior cervical ganglion is regenerative.
Region S2 (secondary somatosensory cortex) divides into Area S2 and parietal ventral area. Area S2 is involved with specific touch perception and is thus integrally linked with the amygdala and hippocampus to encode and reinforce memories. Parietal ventral area is the somatosensory relay to the premotor cortex and somatosensory memory hub, BA5. BA5 is the topographically organized somato memory field and association area.
It is the 2nd most prominent peak in Oregon, after Mount Hood. The nearest peak higher than Sacajawea is Pinyon Peak, in the Rocky Mountains of Idaho, to the east. This makes Sacajawea Peak the 25th most topographically isolated peak of the United States. Sacajawea Peak is the highest summit in the Eagle Cap Wilderness and the Wallowa–Whitman National Forest.
Brindisi and the mostly topographically flat Salento peninsula is subject to light winds during the majority of the year. The two main winds in Salento are the Bora and the Sirocco. The northerly Bora wind from the Adriatic sea is cooling, moderating summer heat and increasing winter wind chill. The southerly Sirocco wind from the Sahara, brings higher temperatures and humidity to Salento.
According to the U.S. Census Bureau, the county has an area of , of which is land and (3.8%) is water. It is the second-smallest county in Nevada by area. The highest point is East Peak at 9,593 ft (2,924 m), while the most topographically prominent mountain is Mount Siegel. Douglas County is in western Nevada in the western United States.
The hills form a compact block consisting of several hill ranges, and contain tangled ridges and ravines running in the northeast and southwest directions, enclosing many narrow valleys (rivers), viz. Kallar, Varattar, Kambalai and Anaimaduvu. Topographically, the area is undulating with an altitude varying from 240 to 1266 m. The rocks on Chitteri hills are chiefly gneisses/granitic in composition.
Adamawa is one of the largest states of Nigeria and occupies about 36,917 square kilometres. It is bordered by the states of Borno to the northwest, Gombe to the west and Taraba to the southwest. Its eastern border forms the national eastern border with Cameroon. Topographically, it is a mountainous land crossed by the large river valleys – Benue, Gongola and Yedsarem.
As far as topographically possible, the temples were freestanding and designed to be viewed from all sides. They were not normally designed with consideration for their surroundings, but formed autonomous structures. This is a major difference from Roman temples which were often designed as part of a planned urban area or square and had a strong emphasis on being viewed frontally.
Carmona 2001, pp. 143–145 ;Moron gate (Puerta de Moron) Topographically the gate was situated close to the slope of San Mateo, leading to the ancient "Little Old Road". Ashlar stone blocks laid without mortar, of a type similar to those of the Puerta de Córdoba, were discovered in a trench dug for work on the modern-day public water supply.
Rocky Mountain foothills near Denver, CO. Foothills or piedmont are geographically defined as gradual increases in elevation at the base of a mountain range, higher hill range or an upland area. They are a transition zone between plains and low relief hills and the adjacent topographically higher mountains, hills, and uplands. Frequently foothills consist of alluvial fans, coalesced alluvial fans and dissected plateaus.
Third Hill Mountain is both the highest and most topographically prominent mountain in Berkeley County within the Eastern Panhandle of West Virginia. Third Hill Mountain reaches its highest elevation of above sea-level southeast of the "Locks-of-the-Mountain" where it "locks" with Sleepy Creek Mountain. The long distance Tuscarora Trail passes along ridge and bench of the mountain.
Its location east of the Aare makes it topographically connected to the Appenzell Alps, by the chain of hills running north of Lake Zurich. View from the crest The mountain is entirely traversed by a trail following the crest from Baden to Dielsdorf. From Dielsdorf a road also leads to Hochwacht, where a radar is operated by Skyguide (municipality of Boppelsen).
And Atoll is biologically and topographically representative of a vast majority of the atolls around Federated States of Micronesia (FSM). It is the most biologically diverse and undisturbed atoll in Pohnpei, Pohnpei's number one marine Area of Biological Significance (ABS) and one of the identified 24 “Priority Action Areas” in the Eco-regional Plan under the National Biodiversity Strategic Action Plan (NBSAP).
Union Street runs across the district roughly west- southwest to east-northeast. Delano and Grand streets are also included in their entirety, and portions of South Bridge, South Clover and South Perry streets are within the district as well. Topographically, the district slopes down towards the river from east to west. All its streets are developed, with a few vacant lots.
North Schell Peak is the highest mountain in the Schell Creek Range of White Pine County, Nevada, United States. It is the ninth-highest mountain in the state, and also ranks as the fifth-most topographically prominent peak in the state. The summit is northeast of the community of Ely within the High Schells Wilderness of the Humboldt-Toiyabe National Forest.
Denali in Alaska is the highest mountain peak of the United States and North America. Denali is the third most topographically prominent and third most topographically isolated summit on Earth after Mount Everest and Aconcagua. This article comprises four sortable tables of mountain summits of the United States that are higher than any other point north or south of their latitude or east or west of their longitude in the U.S. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.All elevations in the 48 states of the contiguous United States include an elevation adjustment from the National Geodetic Vertical Datum of 1929 (NGVD 29) to the North American Vertical Datum of 1988 (NAVD 88).
Toronto's ravines have been presented as central to Toronto's character. Architect Larry Richards describes Toronto as topographically being "San Francisco turned upside down."Fulford, Robert. "The Invention of Toronto: A city defined by its artists", William Kilbourn Lecture, Toronto Historical Board, 12 June 1996 They appear in the works of major Toronto writers such as Margaret Atwood, Anne Michaels, Morley Callaghan and Ann-Marie MacDonald.
Within the context of plate tectonics the city lies at a convergent margin where Nazca Plate in the Pacific is subducted beneath the South American Plate. Topographically Valdivia lies in a depression amidst the Chilean Coast Range. The basement rocks that crops out in the hills around the city are of metamorphic type. The city itself is chiefly built upon terraces made up of hardened volcanic sand.
View towards the Rheinwaldhorn This is a list of mountains of the Swiss canton of Ticino. Ticino is a very mountainous canton and lies almost entirely within the Alps. It is also one of the nine cantons having summits above 3,000 metres. Topographically, the two most important summits of the canton are those of the Rheinwaldhorn (most elevated and isolated) and Monte Tamaro (most prominent).
Topographically, the most important summit of the canton is that of Piz Bernina (most elevated, most prominent and most isolated). Outside the Bernina Range, the Tödi is both the highest and most prominent summit of the canton. This list only includes significant summits with a topographic prominence of at least . There are over 430 such summits in Graubünden and they are found in all its 11 districts.
This is a list of mountains of the Swiss canton of Nidwalden. The list only includes significant summits with a topographic prominence of at least . There are 18 such summits in Obwalden and they are found in almost all its municipalities. Topographically, the three most important summits of the canton are those of the Rotstöckli (most elevated), the Bürgenstock (most prominent) and Pilatus (most isolated).
Topographically, the prefecture consists of three distinct areas. The mountainous western region features the Tanzawa Mountain Range and Hakone Volcano. The hilly eastern region is characterized by the Tama Hills and Miura Peninsula. The central region, which surrounds the Tama Hills and Miura Peninsula, consists of flat stream terraces and low lands around major rivers including the Sagami River, Sakai River, Tsurumi River, and Tama River.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The smallest subdivision in the district, area-wise, has the highest level of urbanisation in the district.
Enclosed Field with Peasant is an example of Van Gogh's late work, where his dynamic brush strokes take control of the paintings. The painting's hurried lines accentuate a vibrant, moving field. The painting seems to pulsate with life, even though only one human is shown. It is the most topographically accurate of van Gogh's four views of a wheat field at the base of the Alpilles.
Many Irish place names are topographically descriptive, and 'Achadh Liathdrom' is no exception. From the western side of the Forth Mountain, as it slopes down towards Ballintlea, a succession of gradual hills and valleys undulate their way across this part of County Wexford towards Camross, Bree and Carrigbyrne Hills. It is on one of these hills or ridges that the village of Taghmon is situated.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south- eastern part of the district. The smallest subdivision in the district, area- wise, has the highest level of urbanisation in the district.
Swinton lies at (53.5122°, -2.3412°), northwest of central London, and west-northwest of Manchester city centre. Topographically, Swinton occupies an area of gently sloping ground, roughly above sea level, and is on the south side of the River Irwell. Swinton lies in the west-central part of the Greater Manchester Urban Area, the UK's second largest conurbation. The M60 motorway passes Swinton on its northwest side.
In December 2010, the Fantozza exploration permit was awarded and published in the Official Bulletin of Hydrocarbons and Geothermal Resources LIV-12. Found in the central Po Valley Basin, the Fantozza concession is a topographically flat area, typical of the Po Valley landscape, again, with exploration targets in the Miocene, Pliocene and Pleistocene turbidites. Deeper targets in the Mesozoic limestone may also be considered.
Nadia district is part of the large alluvial plain formed by the Ganges- Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The smallest subdivision in the district, area-wise, has the highest level of urbanisation in the district.
Apple Orchard Mountain is a peak of the Blue Ridge Mountains in Virginia. Located in Jefferson National Forest, Apple Orchard Mountain is the county highpoint for both Bedford County and Botetourt County, Virginia as well as the highest point on the Blue Ridge Parkway in Virginia. It is also the most topographically prominent mountain in the state. The summit is open, and an FAA radar stands nearby.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The smallest subdivision in the district, area-wise, has the highest level of urbanisation in the district.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat- Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The smallest subdivision in the district, area-wise, has the highest level of urbanisation in the district.
The town of Elzach is located at the eastern border of the district of Emmendingen and borders on the district of the Ortenaukreis and the Schwarzwald-Baar-Kreis. Topographically is the area characterised by the river valley of the Elz and the local hill called Rohrhardsberg. Also Elzach belongs to the Breisgau area and is located at the edge of the Southern Black Forest Nature Park.
December 2018 saw the event move a kilometre east of the original site, to a larger, more topographically diverse space; the fifth edition took place from 13 to 16 December 2018. The sixth edition of Wonderfruit was staged from 12–16 December 2019, with a program stretching from midday Thursday 12 December to the afternoon of Monday 16 December, effectively spanning 99 hours without breaks.
This is a list of hills in the Lake District. To avoid the list becoming infinitely long and arbitrary, only hills with more than 30 m relative height (rising over ) are included. This includes most, but not all, Wainwrights as well as many other hills. Topographically, the boundaries of the Lake District trace the flow of streams from the lowest point between it and the Pennines.
This is a list of the most topographically isolated mountains of Switzerland. This list only includes summits with an isolation of at least , regardless of their elevation or topographical prominence (drop). For a general list of mountains, with height and prominence ranking, see List of mountains of Switzerland. The list includes all eight ultra-prominent peaks of Switzerland as well as several canton high points.
This is a list of mountains of the Swiss canton of Bern. Bern is one of the three cantons (with Valais and Graubünden) having summits above 4,000 metres. It is also one of the two cantons (with Vaud) extending over both the Alps and Jura. Topographically, the most important summit of the canton is that of the Finsteraarhorn (most elevated, most prominent and most isolated).
The distinctive limestone cliffs of Limestack Mountain have been described as "Yosemite-like".Rocky and Steve Reifenstuhl, November 1, 2007, Alaska Stories: 250 Miles 8 Days 300 Million Years Infinite Memories, Nov/Dec 2007 Issue of Mushing Magazine Topographically, "Limestack Mountain" is the highest point in a group of rugged peaks covering ten or more square miles, linked by a series of long, steep ridges.
Topographically lesions may be found on the face, ears, nose, neck, trunk, extremities (including foot pads), perineum and scrotum. Treatment options in SH and CH. SH has proven to be a difficult and frustrating condition to treat. Consequently, many of the early cases were euthanized. Originally we treated dogs with Thymosin (derived from bovine thymus) because of reports of its effectiveness in human LCH cases.
Ward Mountain is the high point of the Egan Range in south-central White Pine County of eastern Nevada. It ranks thirty-fourth among the most topographically prominent peaks in the state. The summit, part of a three mile long crest, is located just south of the city of Ely. The Ward Charcoal Ovens State Historic Park is located on the mountain's eastern flank.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The plains spread southwards from the head of the delta. The Kalyani subdivision has the Bhagirathi on the west, with Hooghly district lying across the river. Topographically, Kalyani subdivision is part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district.
The original name of the town was "Tip Top", chosen for its location on the Missouri-Mississippi Divide and it being Iowa's topographically most elevated town. In 1880, a large fire destroyed most of the business section of Arcadia. Only 2 buildings were spared by the fire. Most of the work for restoring the destroyed buildings was completed within a year after the event.
Local newspaper sources report that Rocky Butte is extinct. Trimble (1963) noted that an eruption at Rocky Butte covered a hill composed of Troutdale Formation rocks, which are exposed as conglomerate rock at a height of on Rocky Butte's western slope. The exposure of rock from the Troutdale Formation suggests that Rocky Butte erupted onto a topographically irregular surface and that this surface later underwent erosion.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The Kalyani subdivision has the Bhagirathi/ Hooghly on the west. Topographically, Kalyani subdivision is a part of the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The smallest subdivision in the district, area-wise, has the highest level of urbanisation in the district.
Draping or blousing is not desirable. This is reserved for much larger breasts or topographically a larger surface area as seen in women with postpartum breast atrophy. The nipple areolar complex may be supported by a pedicle which has the advantage of leaving some sensation and blood supply intact, but can have the disadvantage when the pedicle has sufficient bulk not to provide the flat look most FTM patients desire.
Søften is located within an area defined by a small river valley. The river valley, formed topographically due to Weichselian glaciation during the last Ice Age, and runs along the North and West sides of Søften city. The area is relatively hilly (by Danish standards), with slopes leading towards the river valley north of Søften. The narrow wetland of Damsbro Mose runs along the northeast and southwerst sides of Søften Valley.
After her husband retired in 1939, the family moved back to the Netherlands, in Leiden. There, De Loos-Haaxman published extensively. In addition to historical research, several contributions appeared in genealogical journals and historical-topographically oriented yearbooks. Medal, Knight in the Order of Orange-Nassau On the death of her husband in 1950, De Loos-Haaxman began a long collaboration with her daughter Jeanne Terwen-de Loos (1910–1973).
The Neckar flows through the region for about 90 kilometers, of which about 70 kilometers are navigable waterway. The longest tributary in the region is the Fils (50 km), followed by Murr (45 km), the Rems (35 km) and the Enz (30 km). Topographically the Region lays between 170 m above sea level (Neckar near Kirchheim am Neckar) and 835 m above sea level (swabian albs plateau near Hohenstadt).
This is a list of mountains of the Swiss canton of Obwalden. Obwalden is a very mountainous canton and is one of the nine cantons having summits over 3,000 metres. Topographically, the three most important summits of the canton are those of the Titlis (most elevated), the Brienzer Rothorn (most prominent) and Pilatus (most isolated). This list only includes significant summits with a topographic prominence of at least .
Gullan and Cranston have divided chemical defenses into two classes. Class I chemicals irritate, injure, poison, or drug individual predators. They can be further separated into immediate or delayed substances, depending on the amount of time it takes to feel their effects. Immediate substances are encountered topographically when a predator handles the insect while delayed chemicals, which are generally contained within the insect's tissues, induce vomiting and blistering.
At , Sacajawea Peak is the highest point in the Wallowa Mountains, and the 6th highest peak in Oregon. Matterhorn, another peak in the Wallowa Mountains, is about the same height at Sacajawea Peak, and some sources claim it is actually slightly higher. Sacajawea's prominence of , makes it one of the most topographically prominent peaks in the United States. It is ranked 18th among peaks in the 48 contiguous states.
Cabot is one of the Appalachian Mountain Club's "four-thousand footers", the northernmost in New Hampshire. It is also on the New England Fifty Finest list of the most topographically prominent peaks. The valley of the Israel River separates the Pilot Range from the rest of the White Mountains; Mt. Cabot's relative isolation gives it the fifth-highest topographic prominence in New Hampshire, and the fourteenth-highest in New England.
The cistern is located in Istanbul, in the district of Bakirköy, in the mahalle of Osmaniye, between Fildamı Arkası and Çoban çeşme Sokak, to the northwest of the Veli Efendi horse race track. Topographically, it lies about 2 km west of the Golden Gate of the Walls of Constantinople, in the western part of a small valley - now completely built up - which runs southwards to the Marmara sea.
The Chasseral Pass is located further on the west. The Chasseral is the fourth most topographically isolated mountain of Switzerland, although it is the first when considering only easily accessible summits. This results in a very extensive view over the other mountains of the Jura, the Swiss Plateau, the Alps, the Vosges and the Black Forest. The summit can be reached from the Chasseral hotel, where there is a bus stop.
The lamina terminalis is a layer of gray matter that connects the optic chiasma and the anterior commissure. The septal nuclei are in the septal area, and are essential in generating the theta rhythm of the hippocampus. The dorsal septum projects to the lateral preoptic area, lateral hypothalamus, periventricular hypothalamus and midline thalamus. Fibers from the ventral half of the septum project topographically to the hippocampal formation, thalamus, hypothalamus and midbrain.
Sanjan is an ancient city on the southern edge of the Kara-kum Desert, in the vicinity of the historically eminent oasis-city of Merv. Topographically, Sanjan is located in the Greater Khorasan region of Central Asia. Politically, Sanjan is in the present-day Mary Province of Turkmenistan. Together with Merv, Sanjan was an important stopping place and center of trade on the southern route of the Silk road.
Deeply weathered profiles are widespread on the continental landmasses between latitudes 35°N and 35°S. Conditions for the formation of deeply weathered regolith include a topographically moderate relief flat enough to prevent erosion and to allow leaching of the products of chemical weathering. A second condition is long periods of tectonic stability; tectonic activity and climate change can cause erosion. The third condition is humid tropical to temperate climate.
The Sleeping Giant, long by wide, is located in Hamden with its eastern edge falling into Wallingford. The Giant's profile features distinct "head," "chin," "chest," "hip," "knee," and "feet" sections topographically represented by traprock outcrops and ridge crests. The highest point is the Left Hip, , followed by the Chest, , and the Left Knee and Right Leg, each, and so on. The Giant's Head, , is marked by a cliff.
Several large bays distinctly shape its coast. Boston is the largest city, at the inmost point of Massachusetts Bay, and the mouth of the Charles River. Despite its small size, Massachusetts features numerous topographically distinctive regions. The large coastal plain of the Atlantic Ocean in the eastern section of the state contains Greater Boston, along with most of the state's population, as well as the distinctive Cape Cod peninsula.
Topographically, Budhabare area lies in the upper Terai region of the Indo-Gangetic plains, almost on the foot of the Siwalik hills. It is generally flat in the south, while the northern part is rolling. The area is dissected by two major streams: Biring Khola and Hadiya Khola. Biring Khola runs from north to south along the western border, serving as a natural demarcation between Budhabare and Khudnabari.
The Upper Ore Valley to date has steep sixty-degree valleys or inclines to the north, east and west. The stream cuts right through the lower valley exposing the Ashdown bed in sections along the valley floor. To the west the incline falls off to a plateau which then rises to land level. The North End of the Upper Valley has been topographically mapped to reveal its slopes.
According to the U.S. Census Bureau, the county has an area of , of which is land and (0.09%) is water. The highest and most topographically prominent mountain in the county is Mount Jefferson at 11,949 feet (3,642 m). Nye County is in south-central Nevada. It is Nevada's largest county and the third-largest county in the contiguous United States, after San Bernardino County in California and Coconino County in Arizona.
Topographically, the three most important summits of the canton are those of the Diablerets (most elevated), the Vanil Noir (most prominent) and Mont Tendre (most isolated). The first table lists the highest summits of the canton. It includes all summits above 2,800 metres with a topographic prominence of at least . The seconde table only includes significant summits with a topographic prominence of at least , but has no height cut-off.
The southern, topographically higher portion has a monomodal precipitation pattern. Average temperatures depend on the elevation; the zones at have an average annual temperature of and yearly rainfall of , while the lower altitudes at have temperatures averaging . La Calera at has a total annual precipitation of .Climate-data.org – La Calera The region of the Páramo del Verjón in the eastern part has temperatures between and an annual precipitation of .
Troy Peak is the highest mountain in the Grant Range in northeastern Nye County, Nevada, United States. It is the thirty-sixth highest mountain in Nevada. Troy Peak also ranks as the third-most topographically prominent peak in Nye County and the fourteenth-most prominent peak in the state. The summit is located southwest of the city of Ely, within the Grant Range Wilderness of the Humboldt-Toiyabe National Forest.
This monumental structure was located in the eastern part of the city, close to the river. By the 1880s the population of the city had reached 50,000, and the first public transport service was inaugurated on 3 December 1887. It was commissioned by a man called Charvolin and it connected the station of Besançon-Viotte with the quarter of Tarragnoz, at one edge of the topographically challenging city centre.
While not the highest peak in the Owen Stanley Range (Mount Victoria is the highest), it is the most topographically prominent peak in the range, and it is in fact the third most prominent peak on the island of New Guinea. The peak rises above the timberline, while its lower slopes are well-forested. The Maisin people inhabit the area around Mount Suckling. As of 1972, Mount Suckling had been "very inadequately explored" by Westerners.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro- Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro-Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro- Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro- Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro-Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro- Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro-Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro-Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Mount Davidson is both the highest and most topographically prominent mountain in both Storey County, Nevada, and the Virginia Range. The mountain forms a backdrop for the mining boomtown of Virginia City which was built above the Comstock Lode silver strike. Mount Davidson was named after Donald Davidson, a geologist. Mark Twain mentions a flag on Mount Davidson in his semi- autobiographical book Roughing It. As of 2003 the flagpole was still standing.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo- Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo- Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
This is a list of mountains of the Swiss canton of St. Gallen. The canton of St. Gallen is partially located in the Alps and is one of the nine cantons having summits over 3,000 metres. Topographically, the two most important summits of the canton are those of the Ringelspitz (most elevated and isolated) and the Säntis (most prominent). This list only includes significant summits with a topographic prominence of at least .
Running off north west from the top of Steel Knotts is a truncated ridge which falls quickly over Birkies Knott to valley level. Here the Martindale road is crossed at The Coombes before the land rises again to Hallin Fell, overlooking Ullswater from its fine position between Sandwick and Howtown. Topographically Hallin Fell is the true continuation of Steel Knotts, although the eye naturally gives this distinction to the narrow ridge descending to Howtown.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
Mount Lafayette is a mountain at the northern end of the Franconia Range in the White Mountains of New Hampshire, United States. It lies in the town of Franconia in Grafton County, and appears on the New England Fifty Finest list of the most topographically prominent peaks in New England. The mountain's upper reaches are located in the alpine zone, an area where only dwarf vegetation exists due to the harsh climate.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Deseret Peak is the highest peak in the Stansbury Mountains with an elevation of 11,035 ft. It is located in the Deseret Peak Wilderness area west of Grantsville, Utah and east of Skull Valley Indian Reservation. It is the fourth most topographically prominent peak in the state of Utah. The site is a popular destination for hikers and backcountry skiers as the area is a contrast of the alpine wilderness with the surrounding desert basin.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the upper Indo- Gangetic Plain and Eastern coastal plains. Topographically, the university can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Desatoya Peak is the tallest mountain in both the Desatoya Mountains and Churchill County, in Nevada, United States. It ranks forty-third among the most topographically prominent peaks in the state. The mountain has two peaks with the south peak being the taller at while the north peak has an elevation of . It is located about west of Austin and east of Fallon, along the boundary between Churchill County and Lander County.
Arran's son, Lord Claud Hamilton, is said to have entertained Mary at Craignethan on the night before the Battle of Langside in 1568.This story is questioned by Lindsay (1986), p.164, who suggests that an alternative tale placing Mary at Castlemilk on the eve of the battle, is "topographically more plausible". The battle, at which the Hamiltons fought the forces of Regent Moray, ended in defeat, and Mary was forced to flee to England.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 meters above the mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Topographically, the belt has many superlatives: the highest rate of uplift (nearly 10 mm/year at Nanga Parbat), the highest relief (8848 m at Mt. Everest Chomolangma), among the highest erosion rates at 2–12 mm/yr, the source of some of the greatest rivers and the highest concentration of glaciers outside of the polar regions. This last feature earned the Himalaya its name, originating from the Sanskrit for "the abode of the snow".
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
In the winter they move into the deeply secluded regions. Higher elevation areas are more remote and difficult for humans to access and utilize and other studies have found less deforestation, more reforestation and afforestation, less range contraction, and less extinction in topographically steep areas. All Rhinopithecus species inhabit primary forest and grid cells with tree cover ≥ 75% might constitute important potential habitat. They spend the majority of their life in the trees.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low- lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
The primary mechanism for sedimentation was originally subsidence creating accommodation (space for sediments to accumulate), followed by fault extension and more recently, sediment loading, i.e. the basin continuing to subside because of the weight of sediments within it. The eastern boundary of the main Perth Basin is the Darling Fault, topographically expressed as the Darling Scarp. Small outliers of the Perth Basin, such as the Collie Sub- basin, lie east of the Darling Fault.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
Salcantay, Salkantay or Sallqantay (in Quechua) is the highest peak in the Vilcabamba mountain range, part of the Peruvian Andes. It is located in the Cusco Region, about west-northwest of the city of Cusco. It is the 38th- highest peak in the Andes, and the twelfth-highest in Peru. However, as a range highpoint in deeply incised terrain, it is the second most topographically prominent peak in the country, after Huascarán.
Bokaro district, a part of the Chota Nagpur Plateau, has undulating surface with the altitude varying between 200 and 282 m. Topographically, the entire area is divided into three parts – the Bokaro uplands in the west, the Bokaro-Chas uplands in the middle and Barakar basin in the east. The general slope of the region is from the west to the east. The main rivers are the Damodar, Garga, Parga, Konar and Gobei.
Sitai is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Sitalkuchi is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Mekhliganj is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Haldibari is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
Topographically speaking, Kasur District lies between the river Satluj which flows along its boundaries with India and river Ravi which flows its boundary with Nankana Sahib District. The districts may be divided into two parts, a low lying or riverine area along the two bordering rivers and upland, away from the rivers. The riverine area is generally inundates during monsoon season. The water level in this area is higher than in the upland.
For example, it rises nearly over the edge of the San Luis Valley in only .Blanca Peak on TopoQuest Blanca is also the third most topographically prominent peak in Colorado; it is separated from the higher peaks in the Sawatch Range by relatively low Poncha Pass at . Blanca Peak heads up three major creeks. Holbrook Creek is on the west, flowing from a basin including Crater Lake, Blue Lakes, and Como Lake.
All six rivers flow into the Fuerte River. Each of the six large rivers that flow into the Fuerte River have deep rugged canyons, and these canyons have many ravines and tributaries. Topographically the Copper Canyon region is a very rugged and remote area with few towns and few roads. Going upstream from the Fuerte River on the Chinipas River, there is the town of Chinipas, Chihuahua and further upstream the town of Oteros, Chihuahua.
Spencer is located at (35.743740, -85.458408). The town is situated at the western edge of the Cumberland Plateau, just above the Caney Fork valley. The river forms Van Buren's boundary with White County several miles north of Spencer. US Post Office - Spencer, Tennessee Spencer is topographically isolated by the Cumberland Plateau's escarpment to the north and west, the Cane Creek Valley to the east, and the Dry Fork Gulf to the south.
State Route 305 in the Reese River Valley with the Shoshone Range in the distance According to the U.S. Census Bureau, the county has a total area of , of which is land and (0.5%) is water. The 11,477 ft (3498 m) summit of Bunker Hill, located in the Toiyabe Range near the Nye County border, is the highest point in the county while the county's most topographically prominent peak is Mount Lewis.
During the majority of the Cambrian Period, this basin did not exist. Rather, this part of the Canadian Shield area was still topographically high and emergent. It was only during the later part of the Cambrian that the rising sea level of the Sauk marine transgression slowly submerged it. During the Ordovician, this part of the Canadian Shield continued to be submerged by rising sea levels except for a brief middle Ordovician marine regression.
Bisected by the Raritan River, the county is topographically typical of Central Jersey in that it is largely flat. The majority of the county is located in the Inner Coastal Plain, with the remainder of the county being located on the Piedmont. The elevation ranges from sea level to above sea level on a hill scaled by Major Road/ Sand Hill Road near Route 1 in South Brunswick Township.New Jersey County High Points , Peakbagger.com.
This valley is fully urbanized in the plains, and very busy on its slopes. In the valley it is crossed by the Medellín River, which runs south-north, and its 57 streams throughout its 70 kilometers. Topographically the urban part of the city is a tilted plane that descends from 1600 to 1400 meters above sea level. Bello is in the northern part of the valley and the mountains surrounding the city exceed 2,500 meters.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Holmboe worked as a bailiff (fogd) in Senja and Tromsøe between 1781 and 1800. He made a lasting mark in the region, as he organized settling in the Målselvdalen valley, in what would later become the municipalities of Målselv and Bardu. Farmers from the Gudbrand Valley and Østerdalen moved north mainly between 1791 and 1800, and Jens Holmboe helped about forty families with supplies and funding. Topographically, Målselvdalen was and is similar to Østerdalen.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low- lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
Dolmen from Godavari district, Andhra Pradesh, India. Woodcut from the article "Indiska fornsaker" by Hans Hildebrand. South Asia is the southern region of the Asian continent, which comprises the sub-Himalayan countries and, for some authorities, also includes the adjoining countries to the west and the east. Topographically, it is dominated by the Indian Plate, which rises above sea level as the Indian subcontinent south of the Himalayas and the Hindu Kush.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level.
Crazy Peak () is the highest peak in the Crazy Mountains, an isolated range of the Montana Rockies, in the United States. Crazy Peak dominates the surroundings, rising over above the Yellowstone River Valley, and is the highest peak in Montana north of the Beartooth Mountains, which are to the south. Crazy Peak is also the most topographically prominent peak in Montana. A small glacier exists on the northeast slope of the mountain.
Senaey Khwarram (part of present Banda Daudshah Tehsil, part of Lachi Tehsil and Gumbat area) 3. Barak (present Takht-e-Nasrati Tehsil and Karak Tehsil) Teri State's Barak area was divided into two parts topographically: 1. Tsavatra- Chauntra or the elevated territory (most of Banda Daudshah Tehsil and most of Karak Tehsil) 2. Taal or the sandy plains (Takht-e-Nasrati Tehsil and part of Karak Tehsil, Latambararea) Tsavatra is from the Hindi word Chauntra.
70, Sishu Sahitya SansadThe Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar- Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district. The Churni separates the two plains. A portion of the east forms the boundary with Bangladesh.
The Dürre Wand (literally barren wall) is a mountain ridge in Lower Austria and belongs topographically to the Gutenstein Alps. It stretches from Miesenbach in a WSW direction to the Schneeberg. The Dürre Wand is a ridge, rocky in places, which is bordered by pastures, forests and waterfalls. In contrast to Hohe Wand plateau in the immediate east, it culminates in a narrow ridge-line with its hiking trail offering outstanding views.
According to the 2010 census, Peoria Heights has a total area of , of which (or 38.03%) is land and (or 61.97%) is water. That most of the village is water is due to the fact that most of Upper Peoria Lake lies within its boundaries; this can be seen on official state maps.Peoria Heights map Topographically, the village can be roughly divided into three zones. The Illinois River floodplain, the bluff, and the plateau.
The eastern part of the plateau is covered by two salt deserts, the Dasht-e Kavir (Great Salt Desert) and the Dasht-e Lut. Except for some scattered oases, these deserts are uninhabited. Parts of northwestern Iran are part of the Armenian highlands, which adjoins it topographically with other parts of neighbouring Turkey, Armenia, Azerbaijan, and Georgia. Iran has only two expanses of lowlands: the Khuzestan Plain in the southwest and the Caspian Sea coastal plain in the north.
The border consists essentially of a single straight line orientated NW-SE, from the Saudi tripoint down to the Arabian Sea coast at Ras Darbat Ali. The exception is a small triangular 'kink' roughly halfway along the boundary line, which juts into Yemen so as to include the town of Habarut within Oman. Topographically the border traverses the Rub' al Khali desert in the north and the Jabal Qamar in the Dhofar Mountains in the south.
Idealized ABL structureThe ABL is the lowest part of the Earth's troposphere, loosely about the altitude zone 0 km to 1.5 km. The ABL is the only part of the troposphere directly affected by daily cycled contact with the Earth's surface, so the ABL is directly affected by forcings originating at the surface. Such forcings include: heat flux, moisture flux, convection, friction, pollutant emission, and topographically modified flow. Response times to these forcings typically are an hour or less.
Barbeau Peak on Ellesmere Island is the highest point of Nunavut and the most isolated major summit of Canada. The following sortable table comprises the 150 most topographically isolated mountain peaks of Canada with at least of topographic prominence.This article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence.
Bangladeshi experts have said the massive dam will disrupt the seasonal rhythm of the river and have an adverse effect on downstream agriculture and fisheries. The government of Bangladesh has decided to send an expert team to the dam area to examine the features and likely impact of the dam on the flow of water into the Surma and the Kushiara. Another is the environmental factor. The Tipaimukh area lies in an ecologically sensitive and topographically fragile region.
Shefford County is an historical county in southern Québec, Canada. It is named after Shefford, a small town in Bedfordshire county, England of the same name and is in the Eastern Townships region of Québec. Topographically, part of the county is situated on the western foothills of the Appalachian Mountains. The county contains four small lakes, Lake Waterloo near Waterloo, Lake Boivin in Granby Township, Lake Roxton in Roxton Township, and Lake Stukely in Stukely Township.
However, the competent engineer rejected this and recommended a route though Enkenbach to Hochspeyer, since this was topographically easier. The Hochspeyer–Winnweiler section was opened on 29 October 1870 and on 16 May of the following year the line to Münster was completed. In the beginning, Enkenbach was a stop for long-distance trains towards Neustadt and Kaiserslautern. Although the line connected towards Kaiserslautern at Hochspeyer station, the municipality felt the route through Hochspeyer was inconvenient.
However, rivers typically originate in the highlands, and are slowly created by the erosion of mountain snowmelt into lakes or rivers. Rivers usually flow from their source topographically, and erode as they pass until they reach the base stage of erosion. The scientists have offered a way based on data to define the origin of the lake. A classified sample was the one measured by the Chinese researchers from the University of Chinese Academy of Sciences.
Inverkeithing lies on the north coast of the Firth of Forth, about 10 miles from Edinburgh and 6 miles from Edinburgh Airport. Modern Inverkeithing is almost contiguous with the neighbouring settlements of Rosyth and Dalgety Bay. The nearest larger town is Dunfermline, 4 miles to the northwest. Topographically, Inverkeithing is situated on a raised terrace sloping down towards Inverkeithing Bay, which cuts in to the south of the town, separating it from the North Queensferry peninsula.
The channel tunnels were primarily created by the erosion from glacial rivers, a typical process before moraine formation. Characteristic of this moraine is the transition of deposition layers from glaciofluvial to glaciolacustrine. Sedimentary glaciofluvial areas form the core of the Oak Ridges Moraine, though restricted to subglacial cavity fills of confined subaqueous fans. Overlaying this core is a glaciolacustrine sedimentary layer that is younger and topographically lower, principally in the delta and basin areas of the moraine.
The Hochwald, southwest of Wissembourg The Hochwald is a hill ridge, up to 508 metres high, in the North Vosges in the French département of Bas-Rhin near Wissembourg (German: Weißenburg). Topographically it represents the northernmost part of the Vosges mountains. To the north is the valley of the Lauter, which is both the border between France and Germany (state of Rhineland-Palatinate) and also the boundary between the (North) Vosges and the Palatine Forest (specifically the Mundat Forest).
Red Fescue is one of the dominant species in subcommunity MG5c and is found at Briarcroft Pasture. Briarcrift Pasture, located west of Stockton-on-Tees and close to Whinney Hill, County Durham, is a small site 1.8 hectares (4.4 acres). Topographically the site is level and has an altitude of approximately 50 m and is adjacent to a small stream. The underlying geology of Whitton Bridge Pasture is responsible for shaping the species-rich community found on the surface.
Shaped like a camel's hump, Perry County consists of that fit neatly into a wedge created by the confluence of Apple Creek and the Mississippi River. Topographically, it is divided into lowlands and uplands. The lowlands comprise about one-eighth of the county and lie for the most part along the river. In the northeastern corner is the Bois Brule Bottom, meaning Burnt Wood, the most extensive tract of lowland, approximately long and up to wide.
I, p. 62 Model for restoration of the Temple of Olympian Zeus (by Abel Blouet) As with the excavations led at Messene, the site was divided topographically into squares, trenches were dug, excavations were undertaken in straight lines, and models for restoration were proposed: archaeology was becoming rationalized. The simple treasure hunt was beginning to be abandoned. The fundamental contribution of the Morea scientific expedition was its total indifference towards looting, treasure hunting, and antiquities smuggling.
Nahal Barak in Israel's Southern District is part of a system of streams draining the Arava desert. The Arabah is in length, from the Gulf of Aqaba to the southern shore of the Dead Sea. Topographically, the region is divided into three sections. From the Gulf of Aqaba northward, the land gradually rises over a distance of , and reaches a height of above sea level, which represents the watershed divide between the Dead Sea and the Red Sea.
Of these metal surfaces, copper and zinc have been found to be most effective. Polyurethane, polyethylene glycol, and other polymers have been shown to reduce external bacterial adhesion, which elicits applications of anti-microbial substances to the polymer and coatings industry. Sustainable alternatives like topographically modified cellulose are also of high interest due to recyclability and low cost. Surfaces that are superhydrophobic are desirable for non-fouling behavior because an affinity for water correlates to an affinity for contaminants.
The medial geniculate nucleus divides into ventral (relay and relay-inhibitory cells: frequency, intensity, and binaural info topographically relayed), dorsal (broad and complex tuned nuclei: connection to somatosensory info), and medial (broad, complex, and narrow tuned nuclei: relay intensity and sound duration). The auditory cortex (AC) brings sound into awareness/perception. AC identifies sounds (sound-name recognition) and also identifies the sound’s origin location. AC is a topographical frequency map with bundles reacting to different harmonies, timing and pitch.
The Shfela region within Israel, with inset showing locations of major cities. The Shfela consists of fertile rolling hills. Topographically it represents the transition from the higher and more rugged Jerusalem and Hebron Mountains, whose foothills it forms, and the Coastal Plain. About 60 km (35 miles) long in north-south direction and only 13 km (8 miles) wide, it is subdivided into two parts: the western "Low Shephelah", which starts at an altitude of ca.
The hypothesis of micro-endemism, therefore, states that speciation occurs in small specific habitats as aided by adaptive mechanism occurring in geological, topographical, and climatic isolation. Geologically and topographically, plant populations in xeric climates are broken down into smaller groups. The microclimate responds to the given location transforming it into a habitat. Isolated, the duplicity of organization in Pachypodium form through geology and location significant variation where over evolutionary time a new species might develop, if not have developed.
Mount Logan in the Saint Elias Mountains of Yukon is the highest peak of Canada. The following sortable table comprises the 150 most topographically prominent mountain peaks of Canada. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.If the elevation or prominence of a summit is calculated as a range of values, the arithmetic mean is shown.
In contrast, the dorsal auditory pathway, projecting from the temporal lobe is largely concerned with processing spatial information, and contains receptive fields that are topographically organized. Fibers from this region project directly to neurons governing corresponding receptive fields in V1. The perceptual consequences of this have not yet been empirically acknowledged. However, it can be hypothesized that these projections may be the precursors of increased acuity and emphasis of visual stimuli in relevant areas of perceptual space.
Since it is the highest point in a region which is separated from higher peaks (e.g. in the Sierra Nevada) by relatively low terrain, San Gorgonio Mountain is one of the most topographically prominent peaks in the United States. It is ranked 7th among peaks in the 48 contiguous states and 18th overall. Like other high peaks in the Transverse Ranges, the mountain has a pyramid shape, with a steep north face and a slightly shallower south face.
The surrounding countryside is fertile agricultural land producing grains and providing grazing for cattle. Topographically the region is composed of very gently rolling terrain quite suitable for agriculture. In the 18th century the estate would have amounted to approximately 190 square kilometres. While there were numerous smaller residences on the estate from the 18th century on, in the 19th and 20th century more development has taken place closer to Monboddo House in the form of several single family residences.
Grave Creek Mound, in Moundsville, West Virginia Kościuszko Mound, Kraków, Poland A mound is a heaped pile of earth, gravel, sand, rocks, or debris. Most commonly, mounds are earthen formations such as hills and mountains, particularly if they appear artificial. A mound may be any rounded area of topographically higher elevation on any surface. Artificial mounds have been created for a variety of reasons throughout history, including ceremonial (platform mound), burial (tumulus), and commemorative purposes (e.g.
It is topographically complex with a variety of habitats which include grassland plateaus, wetlands and sponge areas, grassland slopes, afromontane forest, riparian forest, moist woodlands, dry woodlands and shrublands. Its four veld types are Afromontane Forest, North- eastern Mountain Sour Grassland, Sour Lowveld Bushveld and Mixed Lowveld Bushveld. Around a 1,000 plant species have been recorded. This includes cycads, of which the Blyde river cycad is almost endemic to the reserve, with some 200 individuals remaining.
Although he initially produced capricci (i.e. fantastic, imaginary landscapes), he later painted more topographically accurate vedute. One of his patrons was the noted collector Johann Matthias von der Schulenburg, who bought twelve paintings between 1736–38, including two canvases for 50 and 55 gold sequins respectively. He drew on his scenery painting experience to "transform his urban views by using an exaggerated perspective that confers the novelty of a capricious invention even on scenes taken from life".
This is an important distinction as Defining Features must be topographically defensible. Any feature whose existence can be verified through physical evidence can be mapped as a Defining Feature. Features that no longer exist above or below the surface and therefore have no physical trace are still considered battle features but are not mapped as Defining Features. Defining Features not only define the battlefield on the landscape but also serve to pin battle events to identifiable locations.
The western limit touches the limits of Bareilly. According to the Central Statistical Organisation, the district Pilibhit had an area of 3504 km2 on 1 September 2007, occupying 46th position in the state and the total area of the Pilibhit city is 68.76 km2. Pilibhit city, with 2365.11 people per square kilometer, is more densely populated than the rest of the district, which has 469.51 people per km2. The area has diverse features, and topographically may be divided into several distinct tracts.
5th tier at Erawan 7-tier waterfall in Erawan National Park The province is in the west of Thailand, 129 km from Bangkok, and covers a total area of approximately 19,483 km². It is the country's third largest province, after Nakhon Ratchasima and Chiang Mai. Topographically, it is covered with timber and evergreen forests. The district covers the source valleys of the rivers Kwae Yai and Kwae Noi ("River Kwai"), which merge at Kanchanaburi city to form the Mae Klong River.
In the west side, the bedrock underneath the earth is topographically dominant, whereas the other is controlled by Pleistocene and recent deposits leading to the rivers (resulting in the area being shallow and wide). Fredericton and its surroundings are rich in water resources, which, coupled with highly arable soil, make the Fredericton region ideal for agriculture. The Saint John River and one of its major tributaries, the Nashwaak River, come together in Fredericton. The uninhabited parts of the city are heavily forested.
In addition to looking at other computational models of grid cells, Giocomo described the function of head direction cells in the entorhinal cortex in a first author paper in Cell. She found that head direction cells are organized topographically. Specifically, the tuning gradient of these cells decreases along the dorsal to ventral axis and the dorsoventral tuning gradient is only expressed in layer III of the entorhinal cortex. Overall, this paper highlighted the fundamental nature of dorsoventral gradients in entorhinal cortex circuits.
Its other faces drop , all in less than . The toe of the Kuskulana Glacier, less than from the summit, lies at an elevation of , giving a rise of . While these figures speak to the peak's relief, one measure of its independence is that it is the 50th-most topographically prominent peak in the world. The western of Blackburn's two summits is the mountain's highest point, a fact that was not understood until the 1960s when new USGS maps were published.
In the guenon Brodmann area 26 is a subdivision of the cerebral cortex defined on the basis of cytoarchitecture. The smallest of Brodmann's cortical areas in the monkey, it represents cortex that is less differentiated and smaller in monkey and human than in other species. Brodmann regarded it as topographically and cytoarchitecturally homologous to the combined human ectosplenial area 26, granular retrolimbic area 29 and agranular retrolimbic area 30 (Brodmann-1909). Distinctive features (Brodmann-1905): thin cortex; distinct but narrow layers.
Meridian (plural: "meridians") is used in perimetry and in specifying visual fields. According to IPS Perimetry Standards 1978 (2002): "Perimetry is the measurement of [an observer's] visual functions ... at topographically defined loci in the visual field. The visual field is that portion of the external environment of the observer [in which when he or she is] steadily fixating ...[he or she] can detect visual stimuli." In perimetry, the observer's eye is considered to be at the centre of an imaginary sphere.
Topographically this is the Rove Slate Bedrock Complex Landtype Association. The sedimentary and diabase rocks are calcareous; they produce a more basic, nutrient-rich soil compared to the poorer soils typical of the Canadian shield. The Royal River drains Royal Lake [which is about east of South Fowl Lake] into John Lake, both in Minnesota. The relatively rich soils, particularly in the Royal River drainage area, along with steep, moist, north-facing cliffs provide the habitat for these rare plants.
Topographically, the municipality lies in the North Palatine Uplands. The original village of Jettenbach grew in the valley of an eponymous brook, the Jettenbach, from which it took its name. Quite early on, a mediaeval regular route linking Landstuhl to Trier following the nearby ridge running parallel to the brook was established as a roadway. To the south of the village rises the Spannagelberg (449.5 m above sea level) and to the north, the Potschberg (formerly 492 m above sea level).
Garnudden Nature Reserve () is a nature reserve in Salem Municipality, Stockholm County in Sweden. The purpose of the nature reserve is to protect the natural values of the area for the future, as it is located close to an urban environment, as well as an effort to sustain the biodiversity of the area. The area is topographically varied and is typical for forest areas on Södertörn. Several protected species are known from the area, including Phellinus pini and Cortinarius sulfurinus.
The official border between Victoria and Tasmania is at 39°12' S, which passes through Boundary Islet in the Bass Strait for 85 metres. Victoria contains many topographically, geologically and climatically diverse areas, ranging from the wet, temperate climate of Gippsland in the southeast to the snow-covered Victorian alpine areas which rise to almost , with Mount Bogong the highest peak at . There are extensive semi-arid plains to the west and northwest. There is an extensive series of river systems in Victoria.
Construction on the Explorer, a hotel meant to cater to them, began in 1974 and completed in 1976. It was strategically located in a topographically prominent position along the highway leading from the airport to downtown. At that time it had 117 rooms. By the end of the decade the hotel had played host to Prince Charles, who stayed there when he traveled to Yellowknife to speak at the dedication ceremonies for the Prince of Wales Northern Heritage Centre across the road.
El Cobre is a rural town in the municipality of San Martín de Hidalgo in the Mexican state of Jalisco. The town is in between the towns of Lagunillas and Mesa del Cobre, in Sierra de Quila, Jalisco's second-largest forest reserve. The town is topographically settled on top of a mesa with deposits of copper, hence its name of El Cobre, meaning "the copper". El Cobre is the municipality's smallest municipal agency, and counts with 36 inhabitants as of 2010.
Sanandaj A fine old Senneh prayer kilim from the 19th Century Kurdistan Province is a mountainous region that can be topographically divided into a western and an eastern section at Sanandaj. As a result of its elevation and mountains, Kurdistan province has many rivers, lakes, glaciers and caves, which render it rather picturesque. Consequently, Kurdistan has always attracted many tourists and fans of mountaineering, ski and water-sports. The Zarrineh River, 302 km long, is one of the longest rivers of this province.
St Paul's Church Topographically, Halifax is located in the south-eastern corner of the moorland region called the South Pennines. Halifax is situated about from the M62 motorway, close to Bradford and Huddersfield. The Tees-Exe line passes through the A641 road, which links Brighouse with Bradford and Huddersfield, The town lies from Hull and Liverpool, and about from the cities of London, Edinburgh, Belfast, Dublin and Cardiff as the crow flies. The Hebble Brook joins the River Calder at Salterhebble.
Tengchong (labelled as T'eng-ch'ung (T'eng-yüeh) ) (1954) The area of Tengchong is . Situated at the southwestern end of the (transversely faulted) Hengduan Mountains, Tengchong topographically assumes the form of a horseshoe with the opening facing the south. The easternmost sources of the Irrawaddy River issue from the high mountains at the summit of Mount Danaozi of Gaoligong Mountain, above sea level and the lowest point, above sea level, is in the Suqingjiang valley. The elevation of the city seat is .
Jorpatki, a constituent panchayat of this block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Natabari, a constituent panchayat of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Falimari, a constituent panchayat of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Guriahati, one of the constituent panchayats of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Khagrabari, one of the constituent panchayats of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Angarkata Paradubi, a constituent panchayat of this block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Petla, one of the constituent panchayats of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
Sahebganj, one of the constituent panchayats of the block, is located at . Topographically Cooch Behar district is generally plain land which is low and marshy at some places. “Considering the nature of general surface configuration, relief and drainage pattern, distribution of different types of soil, climatic condition, the formation of geology and forest tracts, the district Koch Bihar falls under Barind Tract. The physiology of this area consists of alluvial soil, generally blackish brown in colour and composed of sand, clay and silt.
The River Bleng forms the entire western boundary, beginning on the slopes of Haycock and then flowing out in a huge loop to the south west. It finally joins the Irt and continues on to the sea at Ravenglass. The extremity of the Bleng's circuit, near to Gosforth, is given over to lowland cultivation and although belonging topographically to Seatallan could hardly be termed fellside. Higher up the south western shoulder are conifer plantations, both along the Bleng and above the Irt.
According to various mythographical accounts, not always uniform and coherent, of Strabo, Pseudo-Apollodorus, Lycophron and Pseudo-Aristotle, the Greek hero Philoctetes reached these places on his way back from the Trojan War, together with the Rhodians under Tlepolemus. He colonized the promontory of Crimisa and founded a city of the same name. Topographically, Krimisa was located in a lower area as compared to Chone, city of the Choni, now Cirò. Philoctetes was believed to have also founded Petelia (Strongoli) and Macalla.
Blagaj is one of the most valuable urban-cum-rural structures in Bosnia and Herzegovina. Blagaj reached its peak of development in the 15th and 16th centuries, building in stone also reached its greatest extent. The first stone-built houses were the privilege of the wealthier class, but later, and lower-class families are also built sizeable stone houses and summer residences in large numbers. The natural and architectural ensemble of Blagaj forms a spatially and topographically self-contained ensemble.
Now it is divided into the Italian Riviera and the French Riviera, although the French use the term "Riviera" to refer to the Italian Riviera and call the French portion the "Côte d'Azur". As a result of the fame of the Ligurian rivieras, the term came into English to refer to any shoreline, especially one that is sunny, topographically diverse and popular with tourists. Such places using the term include the Australian Riviera in Queensland and the Turkish Riviera along the Aegean Sea.
The main effect of sodium etching is defluorination of the PTFE, stripping the fluorine molecules from the carbon backbone of the polymer. The fluorine-to-carbon atomic ratio (F/C ratio) is reduced from PTFE's theoretical ratio of 2.0 to 0.2 or less, after exposure to sodium naphthalene for 1 minute. The fluorine atoms are replaced with hydroxyl, carbonyl, and other functional groups which can form hydrogen bonds. Topographically, chemical etching of PTFE with sodium results in a highly porous defluorinated layer.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.1%) is water. It is the fourth-smallest county in Nevada by area. The highest point is approximately 10,565 feet (3,220 m) on the northeast ridge of Middle Sister, the peak of which is located in adjacent Mono County, California, while the highest independent mountain completely within Lyon County is the nearby East Sister. The most topographically prominent peak in Lyon County is Bald Mountain.
The elevation ranges from about at the edge of the salt flats of the Great Salt Lake Desert, to on the summit of Ruby Dome in the Ruby Mountains. The most topographically prominent mountain in Elko County is Pilot Peak. The county has three physiographic sections (70% Great Basin section, 20% Payette, 10% Snake River Plain) and 4 watersheds (45% Humboldt River, 30% Upper Snake River, 20% central Nevada desert, 5% Pilot-Thousand Springs). Lightning-sparked wildfires are common occurrences in Elko County.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (3.7%) is water. The highest point in Washoe County is Mount Rose at 10,785 ft (3,287 m), while the most topographically prominent peak is Virginia Peak. There are two incorporated cities within the county, namely Reno and Sparks. In 2010, there was a ballot question asking whether the Reno city government and the Washoe County government should become one combined governmental body.
Located on the right bank of the Ravi river valley, built on successive flat terraces, the town is bounded topographically by the Dhauladhar and Zanskar ranges, south of the inner Himalayas.Bhatnagar (2008), p.40 Chamba, despite its hill location, is well connected by road to the rest of the state and country, including Shimla, Delhi and Chandigarh along several routes. The nearest broad gauge railway stations are at Chakki Bank and Pathankot, the latter of which is away by road.
Denman Prospect is located to the north of Uriarra Road, west of John Gorton Drive and south of the Molonglo River. Topographically it is north east of Mount Stromlo with a series of valleys draining eastwards towards the Molonglo River in the south of the suburb, and the north east direction in the north. The highest points of the suburb are along hills on the eastern side at just over 654 meters high. Uriarra Road is about 630 m above sea level.
South Asia or Southern Asia is the southern region of Asia, which is defined in both geographical and ethno-cultural terms. The region consists of Afghanistan, Bangladesh, Bhutan, India, the Maldives, Nepal, Pakistan, and Sri Lanka.; ; ; ; ; ; ; ; Topographically, it is dominated by the Indian Plate and defined largely by the Indian Ocean on the south, and the Himalayas, Karakoram, and Pamir mountains on the north. The Amu Darya, which rises north of the Hindu Kush, forms part of the northwestern border.
This occurs just north of the Howgill Fells and gives the boundaries as, primarily, the River Eden and River Lune. This list therefore includes all hills to the west of those rivers including the so-called 'Westmorland Plateau' to the north of the Howgills. Hills are grouped as topographically as possible, according to their 'parent Marilyn'. The parent Marilyn of hill A can be found by dividing the nearby area into territories, by tracing the runoff from the key col of each Marilyn.
Currant Mountain is the highest mountain in the White Pine Range in White Pine County, Nevada, United States. It is the twenty-first-highest mountain in the state, and also ranks as the sixteenth-most topographically prominent peak in the state. Its summit consists of a series of three spires on a thin limestone ridge, with the southern spire being the highest at . To the west are the Duckwater (Shoshone) tribal lands and the northern arm of large Railroad Valley.
Since one of the major characteristics of a surge is the transport of water, measurements of precipitable water and the dew point can also increase. The increased water vapor increases the amount of convective available potential energy (CAPE), which can result in topographically-forced convection. Gulf moisture is typically constrained to central and southern Arizona by the topography of the Mogollon Rim. The moderate steering flow from the surge pushes the convection off the mountains which brings precipitation to the desert valleys.
Nadia district is part of the large alluvial plain formed by the Ganges-Bhagirathi system. The plains spread southwards from the head of the delta. The Ranaghat subdivision has the Bhagirathi on the west, with Purba Bardhaman and Hooghly districts lying across the river. Topographically, Ranaghat subdivision is spread across the Krishnanagar-Santipur Plain, which occupies the central part of the district, and the Ranaghat-Chakdaha Plain, the low-lying area found in the south-eastern part of the district.
The mountain is topographically connected to the Jura Mountains to the west. East of Le Mormont runs the Entreroches gorge (460 m), through which the Canal d’Entreroches was dug in the 17th century, enabling water transportation between the Rhone and the Rhine rivers. The canal ceased to be profitable in the 18th century, and when a bridge across the canal collapsed in 1829, it was shut down altogether. The course of the historical canal is now traversed by a railway tunnel of the Lausanne-Yverdon line.
Mount Elbert in the Sawatch Range is the highest peak of the Rocky Mountains and the highest point in Colorado. The following sortable table comprises the 100 most topographically prominent mountain peaks of the U.S. State of Colorado. Topographic elevation is the vertical distance above the reference geoid, a mathematical model of the Earth's sea level as an equipotential gravitational surface. The topographic prominence of a summit is the elevation difference between that summit and the highest or key col to a higher summit.
Bradford is located at (53.7500, -1.8333)1. Topographically, it is located in the eastern moorland region of the South Pennines. Bradford is not built on any substantial body of water but is situated at the junction of three valleys, one of them, that of the Bradford Beck which rises in moorland to the west, and is swelled by its tributaries, the Horton Beck, Westbrook, Bowling Beck and Eastbrook. At the site of the original ford, the beck turns north, and flows towards the River Aire at Shipley.
Bhitargarh covers an area of , situated in the Amarkhana Union of Panchagarh Sadar Upazila within the Panchagarh District. The site is covered by sand and gravel which flowed down from the Himalayan foothills by glacial waters as well as monsoon rainfalls. Topographically, the land is part of the Old Himalayan Piedmont Plains while the gravel beds belong to the Upper Pleistocene stage, similar to the rest of Panchagarh District. The Upper Pleistocene layer is further overlain by Holocene deposits, evident in the alluvium sand, silt and clay.
Third is attention to detail away from the central focus of the work. For example, in View in the Hills, Hullikkul, one can see that the hills to top left are dotted about with houses, not apparent on a cursory glance, all perfectly positioned, topographically, and in perspective. Capt. Peacocke was trained in surveying in the Army and used this training to good effect in his Neilgherry views. Other than their 1847 publication, the lithographs are undated and the sequence of the original paintings is unknown.
Hole in the Mountain Peak is the highest mountain in the East Humboldt Range of mountains in Elko County, Nevada, United States. It is the thirty-fifth highest mountain in the state, and also ranks as the eleventh-most topographically prominent peak in the state. It is located within the East Humboldt Wilderness of the Humboldt–Toiyabe National Forest and is high. The peak is east of Elko and southwest of Wells, making it a rather prominent feature of the drive along Interstate 80 in Elko County.
Location of Nordenskjöld Coast. Tillberg Peak () is a largely ice-free peak, 610 m, at the northeast extremity of Kyustendil Ridge on the east coast of Graham Land, Antarctica. Situated on the south side of lower Drygalski Glacier, north of Tashukov Nunatak. The name Tillberg was given to a group of four rocky outcrops in this area but, since they are not conspicuous topographically, the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1963 recommended that the name be transferred to this more useful landmark.
Top of South Mountain photographed from the south. The dirt roads on the side lead to active oil wells; most of the oil field is on the other side of the peak. The oil field covers most of the north slope, the summit, and part of the south slope of topographically prominent South Mountain, southeast of Santa Paula. Adjacent to the west and southwest is the small West Mountain Oil Field and the Saticoy Oil Field, which follows the north bank of the Santa Clara River.
The cirque on the southwest gives rise to a Schoharie tributary, the West Kill, also fed by Hunter Brook. Regardless of the stream, all of Hunter is part of New York City's watershed, as the Esopus is impounded in Ashokan Reservoir and the Schoharie in the similarly named reservoir downstream. While Hunter is traversed by the Devil's Path hiking trail and is often considered part of the range of the same name, it is distinct from the Devil's Path topographically due to the fork in the range.
General criticism of Prokop as the central station continued. Member of the Serbian Academy of Sciences and Arts and a public transportation expert, Vukan Vučić labeled Prokop as the "most disastrous error of the Belgrade transportation". He asserted that Prokop, in functional terms, is not a station at all and that, though it has been named Belgrade Center, is actually further from the city's center than the old station was. He added that the location is neglected, desperately bad choice and topographically inaccessible from all sides.
Mt. Susitna is a roche moutonnée, a landform created when a glacier flows over a resistant, topographically high, bedrock body, creating a smooth-sided and teardrop shaped feature aligned with the direction of ice flow. The Anchorage bowl topography has been influenced by 5-7 glaciations. Over several thousand years, thick ice sheets from the Talkeetna, Chugach and Alaska Ranges flowed down Cook Inlet. The five well documented glaciations from oldest to most recent were the Mt Susitna, Caribou Hills, Eklutna, Knik and Naptowne.
The central parts of the steppe are dominated by shrubby and herbaceous plant species albeit to the west, where precipitation is higher, bushes are replaced by grasses.The Physical Geography of Patagonia and Tierra del Fuego. Andrea M. J. Coronato, Fernando Coronato, Elizabeth Mazzoni and Mirian Vazquez Topographically the deserts consist of alternating tablelands and massifs dissected by river valleys and canyons. The more western parts of the steppe host lakes of glacial origin and grades into barren mountains or cold temperate forests along valleys.
Cerro Amay is a mountain in the Quiché Department of Guatemala, centered near -90.77 W, 15.48 N. The mountain is affiliated with, but not part of, the Cuchumatanes Mountains, which lie to its west, and with the Sierra De Chama. Cerro Amay is topographically-distinct and is notable for the Cerro Amay Cloud Forest, a track of mostly virgin cloud forest covering approximately 19,000 hectares. Cerro Amay gets its name from Spanish and Kek'chi, a Mayan language. Cerro means 'mountain' and Amay means 'difficult to survive.
The Zapata Swamp lies between 22°01’ and 22°40’ N latitude and between 80°33’ and 82°09’ W longitude. The swamp in total is over one million acres (4,000 km²). Topographically, the maximum height above sea level is only about 10 meters with the top depth in below-sea-level coastal zones as follows: 2 meters in the salt-marsh area and from 1-600 meters in the sea coastal zone. Between May and October, the warmest season of the year, average temperature is .
Mummy Mountain from Cathedral Rock trail Mount Charleston, including Charleston Peak (Nuvagantu, literally "where snow sits", in Southern Paiute) at , is the highest mountain in both the Spring Mountains and Clark County, in Nevada, United States. It is the eighth-highest mountain in the state. Well separated from higher peaks by large, low basins, Charleston Peak is the most topographically prominent peak in Nevada, and the eighth-most-prominent peak in the contiguous United States., It is one of eight ultra-prominent peaks in Nevada.
Topographically the land in the area is flat, being in the Mersey valley region (other than where man-made features such as the railway bridge have enforced changes). Padgate Brook, a tributary of the Mersey, runs to the western edge of Padgate, it is in turn fed by numerous smaller waterways (Spittle Brook, Blackbrook, Spa Brook, Cinnamon Brook, Cross Brook, Cockshot Burn) originating in Peel Hall Meadows and other outlying rural stretches of land to the north of the district. To the east, Birchwood Brook also feeds the Mersey.
Although the Netherlands seems to be a tectonically quiet area, a number of fault activities have been shown in the past. The latest strong earthquake, the 1992 Roermond earthquake (5.4 on Richter scale), had its epicenter close to the Limburg city of Roermond. The south of the Netherlands is topographically higher and is linked to the geology of the Ardennes and the London-Brabant Massif. The Lower Rhine Graben, part of the European Cenozoic Rift System, which has been tectonically active since the Oligocene, affects the southwestern part of the Netherlands.
This bluff was, at the time of original settlement, divided by ravines through which various creeks flowed, ravines which have been mostly filled in as the city grew. Sheridan Hollow, just north of downtown, was an exception as it could not be completely filled and still topographically sets off Arbor Hill and the Tivoli Nature Preserve to its north.Waite, 104. With the exception of the riverfront portion of the city, Interstate 90 roughly parallels the city's northern boundary with the village of Menands and, further inland, the town of Colonie.
Oxford University Press, 1912 Since the 1950s when the village expanded there have been two parts to the village: Cubbington proper which was the old village core, and New Cubbington which is to the west, although both are referred to as Cubbington. Topographically the highest point of the village sits about above sea level while its lowest is about . For many years the electorate for Cubbington was represented in government by the Member of Parliament for Warwick and Leamington but for the 2010 UK Elections it moved to the new Kenilworth & Southam constituency.
These plantations were developed primarily in the southernmost reaches of the county, in the lowlands along the banks of the Tombigbee River and stretching over a small prairie-like area. The rest of the county was settled by yeomen farmers who held few slaves; it was topographically unsuited for plantation-scale farming operations. During the American Civil War, the first courthouse in Carrollton was burned on April 5, 1865, by troops of Union General John T. Croxton. Recovering from that and other damage was part of the postwar work for the county.
According to the recent study by Box and Fujiwara (Evergreen Broadleaved Forests of the Southeastern United States: Preliminary Description), laurel forests occur in patches in the southeastern United States from southeast Virginia southward to Florida, and west to Texas, mostly along the coast and coastal plain of the Gulf and south Atlantic coast. In the southeastern United States, evergreen Hammock (ecology) (i.e. topographically induced forest islands) contain many laurel forests. These laurel forests occur mostly in moist depression and floodplains, and are found in moist environments of the Mississippi river basin to southern Illinois.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
On the 16th, warm air picking up moisture – due to residual heat from the Atlantic Ocean – travelled towards the South West Cornish coast as prevailing winds. Upon contact with the topographically vertical coast, these winds experienced a strong up-drafting force thus causing internal moisture to reach the atmosphere, and consequently cool as a string of storm clouds. With convergence and coalescence, enhanced moisture levels resulted in heavy rainfall on the afternoon of 16 August 2004. 185 mm (7 inches) of rain fell over the high ground just inland of Boscastle.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
Although of only modest elevation, the isolation of the Belknap Mountains gives Belknap Mountain of relative height above the low ground separating it from the White Mountains, making it one of the fifty most topographically prominent peaks in New England. Belknap Mountain is flanked to the northwest by Gunstock Mountain, the site of the Gunstock Mountain Resort ski area. The summit of Belknap Mountain features an active fire tower. Belknap Mountain stands within the watershed of the Merrimack River, which drains into the Gulf of Maine in Massachusetts.
Brodmann area 6 is a cytoarchitecturally defined portion of the frontal lobe of the guenon. Brodmann-1909 regarded it as topographically and cytoarchitecturally homologous to the human agranular frontal area 6 and noted that, in the monkey, area 4 is larger than area 6, whereas, in the human, area 6 is larger than area 4. Distinctive features (Brodmann-1905): It is thick relative to other cortical areas; the transition from cortex to subcortical white matter is gradual; cell layers are indistinct; and the internal granular layer (IV) is absent.
West Spanish Peak is the easternmost 4000 meter (13,123 ft) mountain peak in the United States. Due to its position well east of the Culebra Range and on the edge of the eastern plains of Colorado, West Spanish Peak enjoys great local vertical relief in almost all directions. For example, it rises over 6,000 ft (1,828 m) in less than 6.5 miles (10.5 km) on both its north and south flanks. Though not a fourteener, West Spanish Peak is the twelfth most topographically prominent peak in the state.
The ridge of Vorberge is located in the eastern edge of the Leine Uplands in the Lower Saxon Hills. It lies between the town of Alfeld on the River Leine to the southwest and Sibbesse on the Alme to the north. The Vorberge is surrounded by other uplands: the Hildesheim Forest to the north, the Sauberge to the east- northeast, Harplage to the east-southeast, the Heber to the southeast, the Sackwald to the south and the Sieben Berge to the west. Topographically, it transitions seamlessly to the last named range.
Har Qatum, a mesa located on the southern edge of Makhtesh Ramon, Israel Mesas form by weathering and erosion of horizontally layered rocks that have been uplifted by tectonic activity. Variations in the ability of different types of rock to resist weathering and erosion cause the weaker types of rocks to be eroded away, leaving the more resistant types of rocks topographically higher than their surroundings. This process is called differential erosion. The most resistant rock types include sandstone, conglomerate, quartzite, basalt, chert, limestone, lava flows and sills.
City of Bhubaneswar from Khandagiri hill The city is bounded by the Daya River to the south and the Kuakhai River to the east; the Chandaka Wildlife Sanctuary and Nandankanan Zoo lie in the western and northern parts of Bhubaneswar, respectively. Bhubaneswar is topographically divided into western uplands and eastern lowlands, with hillocks in the western and northern parts. Kanjia lake on the northern outskirts, affords rich biodiversity and is a wetland of national importance. Bhubaneswar's soils are 65 per cent laterite, 25 per cent alluvial and 10 per cent sandstone.
As they are all inland cities, biblical commentator A. W. Streane argues that the wording There is trouble [or anxiety] on the sea "is quite unsuitable topographically to this context", preferring to translate this line as "because of care, like the sea, they cannot rest" (S. R. Driver's translation).Driver, S. R. (1906), The Book of the Prophet Jeremiah, p.296Streane, A. W., Cambridge Bible for Schools and Colleges on Jeremiah 49, accessed 18 April 2019 Similarly, the Good News Translation has "anxiety rolls over them like a sea, and they cannot rest".
Gawler is the oldest country town on the Australian mainland in the state of South Australia. It was named after the second Governor (British Vice-Regal representative) of the colony of South Australia, George Gawler.History of Gawler 'Shawfactors' It is about north of the centre of the state capital, Adelaide, and is close to the major wine producing district of the Barossa Valley. Topographically, Gawler lies at the confluence of two tributaries of the Gawler River, the North and South Para rivers, where they emerge from a range of low hills.
The combining form laim- from (Greek: λαιμός) denotes a connecting organ (neck) while -sphere indicates a zone of influence. Topographically, the laimosphere includes the soil around any portion of subterranean plant organs other than roots where exuded nutrients (especially sugars and amino acids) stimulate microbial activities. Subterranean plant organs with a laimosphere include hypocotyls, epicotyls, stems, stolons, corms, bulbs, and leaves. Propagules of soil-borne plant pathogens, whose germination is stimulated by a plant exudates in the laimosphere, can initiate hypocotyl and stem rots leading to "damping-off".
To the east is the large open lawn of John Paulding School, the public elementary school of the Union Free School District of the Tarrytowns, which has its headquarters north of the school in the former Edward Harden Mansion, also listed on the National Register. Behind them runs the Old Croton Aqueduct, a National Historic Landmark. The commercial areas of downtown Sleepy Hollow are two blocks to the north along North Broadway. Topographically the park consists of two slight rises, more pronounced toward the west, reflecting the land's general descent toward the nearby Hudson River.
Surface water becomes critical in the dry season The Yala area is mostly composed of metamorphic rock belonging to the Precambrian era and classified into two series, Vijayan series and Highland series. Reddish brown soil and low humic grey soil are prominent among six soil types. Yala is situated in the lowest peneplain of Sri Lanka, which extends from Trincomalee to Hambantota. Topographically the area is a flat and mildly undulating plain that runs to the coast with elevation is close to the coast while rising in the interior to .
The terrain of Churchill County consists of rugged mountainous ridges, dotted with lakes and ponds.Churchill County NV Google Maps (accessed 10 February 2019) The county's east and west sides are higher than the intermediate valley; its highest point around the county periphery is a ridge on the lower east boundary line, at 9,380' (2859m) ASL. The county has an area of , of which is land and (1.9%) is water. The county's highest point is Desatoya Peak at 9,977' (3041m), while the most topographically prominent peak is Mount Augusta, at 9,970' (3039m) ASL.
The embayment is a topographically low-lying basin that is filled with Cretaceous to recent sediments. The northern end of the embayment appears as an anomalous break in regional geologic structure with Paleozoic sedimentary rocks both to the east in Kentucky and Tennessee and to the west in Missouri and Arkansas. The current sedimentary basin results from the filling of a Cretaceous tectonic basin and existed as a large bay in the Cretaceous through early Cenozoic shoreline. The New Madrid Seismic Zone lies at the northern end of the embayment.
The regolith of a region is the product of its long weathering history; leaching and dispersion are dominant during the initial phase of weathering under humid conditions. Saprolites form in high rainfall regions which result in chemical weathering and are characterised by distinct decomposition of the parent rock's mineralogy. Conditions for the formation of deeply weathered regolith include a topographically moderate relief flat enough to allow leaching of the products of chemical weathering. A second condition is long periods of tectonic stability; tectonic activity and climate change partially erode the regolith.
The castle is especially well known for its surrounding rococo garden. In the 19th century this park, which was then a public facility, was nearly destroyed by the construction of the railway. Engineers had planned to use the central avenue of the park for the trackbed of the railway.Eckhart Rüsch: Der Bahnhof Veitshöchheim, in Jahrbuch für Eisenbahngeschichte 24 (1992), S. 23ff This idea was however vetoed by King Ludwig I, who ordered the line to be routed to the east around the castle gardens even though this was topographically less suited.
Wheeler Peak is the tallest mountain in the Snake Range and in White Pine County, in Nevada, United States. The summit elevation of makes it the second- highest peak in Nevada, just behind Boundary Peak. With a topographic prominence of , Wheeler Peak is the most topographically prominent peak in White Pine County and the second-most prominent peak in Nevada, just behind Mount Charleston. The mountain is located in Great Basin National Park and was named for George Wheeler, leader of the Wheeler Survey of the late 19th century.
A separate branch, the Apuan Alps, goes to the southwest bordering the coast south of La Spezia. Whether they are to be considered part of the Apennines is a matter of opinion; certainly, they are part of the Apennine System. Topographically only the valley of the River Serchio, which running parallel to the coast turns and exits into the Tyrrhenian Sea north of Pisa, separates the Apuan Alps from the Apennines; geologically the rock is of a slightly different composition: marble. The Roman marble industry was centered at Luna, and is now active in Carrara.
Botswana is topographically flat, with up to 70 percent of its territory being the Kalahari Desert. It is bordered by South Africa to the south and southeast, Namibia to the west and north, and Zimbabwe to the northeast. Its border with Zambia to the north near Kazungula is poorly defined but is, at most, a few hundred metres long. A mid-sized country of just over 2.3 million people, it is one of the most sparsely populated countries in the world. Around 10 percent of the population lives in the capital and largest city, Gaborone.
According to a report on wetland protection, “All floodwaters come from the Garo/Meghalaya Hills through a number of hill streams and rivers. These in turn eventually drain out of the area through the Kaliganga-Kangsha River, which is part of the Sylhet Basin Haor complex of rivers and streams. Topographically a low-lying plain generally sloping from the north-west to south-east, this site was once a large lake. Presently the wet season water area is about 82.1 square kilometres with a dry season water area of about 9 square kilometres.
Topographically, Wyandanch's nutrient-poor loam and sandy soils are part of the outwash plain which was formed as the last glacier melted about 10,000 BCE. The outwash plain slopes gently towards Belmont Lake State Park from the Half Way Hollow Hills terminal moraine and from Little East Neck Road. In the mid and late 20th century, the Wheatley Heights area (Half Hollow Hills School District) developed as a separate community (due to class and racial dynamics) but is still served by the Wyandanch Fire Department and the US Postal Service.
The start of the fault in the west is assessed as being near Oschatz, but it first becomes topographically significant as a steep ledge near Weinböhla. From there it runs eastwards along the northern perimeter of the Dresden Basin and forms the Elbe valley slopes from Radebeul via Dresden to Pirna. From there it continues rather less noticeably along the northern edge of the Elbe Sandstone Mountains via Hohnstein and Hinterhermsdorf. In Hohnstein by the so-called Wartenberg Road (Wartenbergstraße) is the only geological outcrop where the granite of Lusatia lies immediately above the sandstone.
It is a geomorphological subsystem of the Alps-Himalaya system, specifically a sediment-filled back-arc basin which spread apart during the Miocene. Most of the plain consists of the Great Hungarian Plain (in the south and east, including the Eastern Slovak Lowland) and the Little Hungarian Plain (in the northwest), divided by the Transdanubian Mountains. The Pannonian Basin lies in the southeastern part of Central Europe. It forms a topographically discrete unit set in the European landscape, surrounded by imposing geographic boundaries - the Carpathian Mountains and the Alps.
Pico da Bandeira is also remarkable for being the Brazilian mountain with the greatest topographic isolation: 2,344 km (1,457 miles). This means that at less than that distance, there is no other point on the surface of the Earth at equal or greater elevation. In the Americas, only Aconcagua, Denali, Pico de Orizaba and Mount Whitney are more topographically isolated than Pico da Bandeira, and in the entire world, there are only 20 more isolated mountains. It is one of the major attractions of Caparaó National Park (), accessible from the nearby town of Alto Caparaó.
Ward first published the story as a series of 16-page periodicals in 1698–1700, comprising 18 folio editions. They were printed as a collection in book form in 1703 by J. How of Gracechurch Street, London, a mile from where Ward had his public house. The parts are arranged topographically, the story being told in the first person by the author under the persona of "The London Spy". It concerns his adventures as an ostensibly innocent country gentleman visiting London, his native-Londoner chaperone-cum-guide, and the adventures that befall them.
The town of Sebnitz lies in the valley of the River Sebnitz and its side valleys between 251 and 460 m above sea level between the mountains of Saxon Switzerland and the Lusatian Highlands. Topographically the town itself lies in the West Lusatian Upland, but lies right on the border with the Upper Lusatian Highlands. Because the natural region of Saxon Switzerland is also very close by, the countryside around the town is very varied. The local hill of Sebnitz is the Tanečnice (Tanzplan) which is on Czech territory.
Closer view of Ruby Dome from the trail to the summit Ruby Dome is the highest mountain in both the Ruby Mountains and Elko County, in Nevada, United States. It is the twenty-seventh-highest mountain in the state, and also ranks as the thirteenth-most topographically prominent peak in the state. The peak is located about southeast of the city of Elko within the Ruby Mountains Ranger District of the Humboldt-Toiyabe National Forest. The mountain rises from a base elevation of about to a height of .
The iliopsoas consists of psoas major (and occasionally psoas minor) and iliacus, muscles with separate origins but a common insertion on the lesser trochanter of the femur. Of these, only iliacus is attached to the pelvis (the iliac fossa). However, psoas passes through the pelvis and because it acts on two joints, it is topographically classified as a posterior abdominal muscle but functionally as a hip muscle. Iliopsoas flexes and externally rotates the hip joints, while unilateral contraction bends the trunk laterally and bilateral contraction raises the trunk from the supine position.
Farm in Carroll County, Maryland According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.1%) is water. Topographically, Carroll County is located within the Piedmont Plateau region, with characteristic upland terrain of rolling hills and deciduous forest. The most prominent relief is Parr's Ridge, which bisects the county from southwest to northeast. The highest point is an unnamed hilltop a half-mile south of the Pennsylvania state line in the northeastern part of the county off Harvey Yingling Road.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
The dorsomedial area (DM) also known as V6, appears to respond to visual stimuli associated with self- motion and wide-field stimulation. V6, is a subdivision of the visual cortex of primates first described by John Allman and Jon Kaas in 1975. V6 is located in the dorsal part of the extrastriate cortex, near the deep groove through the centre of the brain (medial longitudinal fissure), and typically also includes portions of the medial cortex, such as the parieto-occipital sulcus (POS). DM contains a topographically organized representation of the entire field of vision.
Along with Rubens, Teniers was among the first Flemish 17th-century artists to include rainbows in his compositions, not for their religious or allegorical meaning, but rather as another means by which to showcase his careful study of nature. Other examples of this include other works from the mid 1640s such as The Reaping (Hermitage Museum).David Teniers (II), River landscape with rainbow at Sotheby's Teniers depicted real as well as imaginary landscapes. Although he did not intend these works to be topographically accurate, he spent a lot of time sketching in the countryside.
Great Basin National Park is an American national park located in White Pine County in east-central Nevada, near the Utah border, established in 1986. The park is most commonly entered by way of Nevada State Route 488, which is connected to U.S. Routes 6 and 50 by Nevada State Route 487 via the small town of Baker, the closest settlement. The park derives its name from the Great Basin, the dry and mountainous region between the Sierra Nevada and the Wasatch Mountains. Topographically, this area is known as the Basin and Range Province.
The south face of the church in Saint-Pardoux-la-Rivière with its sun dial The commune's territory is divided into two contrasting domains by two crossing fault lines (N 065 and N 160). To the north and east of these faults one encounters the Variscan basement rocks of the northwestern Massif Central, which also stand out topographically. The southern lowlands around the village center are occupied by sediments of the northern Aquitaine Basin. Along the border faults the basement rocks were raised relative to the sedimentary cover.
The county is part of the Delmarva Peninsula as well as Maryland's "Eastern Shore." Topographically, Cecil County straddles the border between the rolling hills of the Piedmont Plateau north of U.S. Route 40 and the flatlands of the Atlantic Coastal Plain to the south. The highest and most rugged hills are found in the northwestern and north-central parts of the county, reaching just south of the Mason–Dixon line near Nottingham, Pennsylvania and just east of U.S. Route 1. The lowest elevation is sea level along the Chesapeake Bay.
Blair, Don: Exploring Lakeland Tarns: Lakeland Manor Press (2003): The outflow is to Ullswater to the north east, picking up all of the rainfall from the eastern face of Dollywaggon Pike. To the west of the tarn is the unnamed col between Dollywaggon Pike and Seat Sandal and immediately to the south is Grisedale Hause, the depression between Seat Sandal and Fairfield. Thus Seat Sandal stands topographically on the ridge between the two higher fells, but so out on a limb that many walkers proceed directly from Dollywaggon Pike to Fairfield.
This is short for 'Serenissorum Archiducum Pictor', a reference to his official position as a court painter to Archduke Albert and Archduchess Isabella.Denis van Alsloot, Flight into Egypt at Sotheby's Van Alsloot painted topographically accurate as well as imaginary landscapes, including summer and winter landscapes. Like later landscape painters in Brussels such as Lucas Achtschellinck, Lodewijk de Vadder and Jacques d'Arthois, van Alsloot drew inspiration from the Sonian Forest near Brussels. His forested landscapes often incorporate views of castles and abbeys located in the Sonian Forest near Brussels.
Križevci lies on 140 m above the level of the sea, where the southern part of Kalnik begins. Topographically, it lies on pleistocene surface, between swamped alluvial valleys of the brook Vrtlin from the east and the brook Koruska from the west. Relief, geological-petrografical structure, convenient climate and abundance of water, all these were elements of economical and demographic development of the city. Modern demographic- economical transformation has changed relations in space and structure of population, and it is observable through processes of deagrarization, industrialization and deruralization.
Actin filaments are also possibly involved in guiding the phragmoplast to the site of the former preprophase band location at the parent cell wall. While the cell plate is growing, segments of smooth endoplasmic reticulum are trapped within it, later forming the plasmodesmata connecting the two daughter cells. The phragmoplast can be differentiated topographically into two areas, the midline that includes the central plane where some of the plus-ends of both anti-parallel sets of microtubules (MTs) interdigitate (as in the midbody matrix), and the distal regions at both sides of the midline.
The key terrain feature of Northern Germany is the North German Plain including the marshes along the coastline of the North and Baltic Seas, as well as the geest and heaths inland. Also prominent are the low hills of the Baltic Uplands, the ground moraines, end moraines, sandur, glacial valleys, bogs and Luch. These features were formed during the Weichselian glaciation and contrast topographically with the adjacent Central Uplands of Germany to the south, such as the Harz and Teutoburg Forest, which are occasionally counted as part of Northern Germany.
The woman appears to be hiding from a pair of figures in the distant background; the green christ providing her cover from the figures. Topographically, the site depicted is the Atlantic coast at Le Pouldu. But the calvary depicted is an amalgam of calvaires from different site; the cross is based upon that in the centre of Névez, a community close to Pont-Aven and several miles from the coast, and the figure of Christ is based upon the calvaire at Briec - also some distance from the sea.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
The district is essentially rectangular in shape, covering both sides of Delavan Terrace and the lots at the corners on Palisade and Park Avenues. An extension at the southwest includes the now-vacant lot where the Smith–Collins House stood on the west side of Palisade. The total area is . Topographically the street is on the south end of a ridge between the Hudson River a half-mile (1 km) to the west and one of its tributaries, the Saw Mill River, the same distance to the east.
Azoria is an archaeological site on a double-peaked hill overlooking the Gulf of Mirabello in eastern Crete in the Greek Aegean. "Azoria" (o Αζοριάς or (c. 1900) Μουρί τ' Αζωργιά)Boyd 1901 is a local toponym, not apparently an ancient place name or epigraphically-attested Greek city. View of Azoria from the Kastro with the Kavousi plain and Bay of Mirabello, with the island of Pseira, in the background Located about 1 km southeast of the modern village of Kavousi, and 3 km from the sea, the site occupies a topographically strategic position (c.
It is a register of all the long-term leases the abbey issued, intended to complement the Regestum's catalogue of itsfixed ("hereditary") possessions. These massive volumes were not easy to use for the monastery's agents in property disputes, and so, when already in his seventies (in the early 1130s), Gregory composed the Liber floriger chartarum coenobii pharphensis, an index of all the abbey's properties organised topographically by churches and estates.Biblioteca Nazionale, MS Farfense 3. Gregory's Liber floriger has been superseded by the indices of the modern editors of Farfa's charters.
A short length at the northern end of the road is tarred but contains no kerbs or gutterings. A number of informal sidetracks and turning circles have been formed along the eastern side of the road over the sand dunes. There are a number of 4WD roads and numerous walking tracks between the boulevard and the beach at the northern end of the beach. The southern end of the beach, from the carpark to the end of the beach, is flanked by steep rocky slopes and rocky bluffs which topographically prohibits access to the beach.
Purba Medinipur district is part of the lower Indo-Gangetic Plain and Eastern coastal plains. Topographically, the district can be divided into two parts – (a) almost entirely flat plains on the west, east and north, (b) the coastal plains on the south. The vast expanse of land is formed of alluvium and is composed of younger and coastal alluvial. The elevation of the district is within 10 metres above mean sea level. The district has a long coastline of 65.5 km along its southern and south eastern boundary.
Vertically aligned periodic arrays of carbon nanotubes (CNTs) are used to create topographically enhanced light-trapping photovoltaic cells. The CNTs form the back contact of the device and serve as a scaffold to support the photoactive heterojunction. Molecular beam epitaxy is used to deposit CdTe and CdS as the p/n-type materials and ion-assisted deposition is used to deposit a conformal coating of indium-tin oxide as the transparent top contact. Photocurrent produced “per cm2 of footprint” for the CNT-based device is 63 times that of a commercially available planar single crystal silicon device.
The ESA SMART-1, NASA Clementine and JAXA SELENE spacecrafts made maps of the lunar poles that have been used to identify sites receiving eternal light. The orbiting craft monitored the lighting at the poles and looked for seasonal variations, as well as mapping the relief so that peaks of eternal light could be identified topographically. The Lunar Reconnaissance Orbiter then took a data set including 24,000 wide-area camera and 31,500 narrow-angle camera images within 2° of the poles. These were used to construct high-resolution maps that reveal illuminated terrain under varying lighting conditions.
Differential erosion enhances relief, as clear in this incredibly steep-sided Norwegian fjord. Because ice can flow faster where it is thicker, the rate of glacier-induced erosion is directly proportional to the thickness of overlying ice. Consequently, pre-glacial low hollows will be deepened and pre-existing topography will be amplified by glacial action, while nunataks, which protrude above ice sheets, barely erode at all – erosion has been estimated as 5 m per 1.2 million years. Non- technical summary: This explains, for example, the deep profile of fjords, which can reach a kilometer in depth as ice is topographically steered into them.
The Kettleman North Dome occupies the northernmost portion of the Kettleman Hills, a northwest-southeast trending line of hills about long which parallels the San Andreas Fault to the west. The range consists of two elongate "domes", the North Dome and Middle Dome; a portion of the Middle Dome is sometimes called the "South Dome," although the North and Middle Dome are the most topographically distinct. Both the North and Middle Domes overlie oil fields. The Kettleman Hills is named, and misspelled, after Dave Kettelman, a pioneer sheep and cattle rancher who grazed his animals there in the 1860s.
Topographically one of the lowest points in New Orleans, Broadmoor suffered extensive damage due to Hurricane Katrina. In 2006, the neighborhood was deemed a drainage point in the city's reconstruction plan under the Bring New Orleans Back Commission that was led by former mayor Ray Nagin. The proposal was met with strong opposition as residents rallied to save their neighborhood from disinvestment and destruction. The Keller Library became an important symbol of Broadmoor and a natural locus for redevelopment efforts with the Broadmoor Improvement Association, founded in 1930, touting the notion of an education corridor as central to its neighborhood vision.
From the 3rd century comes a rare funerary monument in Greek, considered by some to be Christian ', and a hoard of coins of Claudius Gothicus (268-270 CE) discovered in a bath sewer. Imported terra sigillata and glassware form a continuous series between late Augustan wares (early Hispanic) and late African D, late Gallic and Focean, with the latest pieces dated from the 7th century. The overwhelming volume peak corresponds to South Gallic wares of the 1st century CE but the studied material is much limited topographically. Fish preserve industries are well documented in the town and neighbourhood, as well as amphorae factories.
Kuh-e Bandaka (Pashto: کوه بندکا) or Kohe Bandaka, Koh-i Bandaka, Bandako, or incorrectly Koh-i-BandakorRobin Hartshorne, "Bandako", American Alpine Journal, 1966.) is one of the highest peaks of the Hindu Kush mountain range in northeastern Afghanistan. It is northeast of Kabul and west of Chitral. Separated by a relatively low pass from the core of the Hindu Kush, it is the second highest mountain entirely within Afghanistan, and the most topographically prominent peak in all of Afghanistan. On September 22, 1960, the second German expedition to visit the Hindu Kush made the first ascent of Kuh-e Bandaka.
These glutamatergic inputs are generally topographically arranged such that the putamen takes information largely from the sensorimotor cortex whereas the caudate nucleus obtains information largely from the association cortex. In addition, the dorsal striatum receives excitatory inputs from other brain structures like the thalamus, and minor excitatory inputs from the hippocampus and amygdala. The dorsal striatum contains neurochemically defined compartments called striosomes (also known as patches) that exhibit dense μ-opioid receptor staining embedded within a matrix compartment that contains higher acetylcholinesterase and calbindin-D28K. The dopaminergic axon terminals of the nigrostriatal pathway synapse onto GABAergic MSNs in the dorsal striatum.
Topographically, the Romanche basin (a tributary of the Isère river) is a particularly deep valley. Situated between Grenoble and Italy, it is one of the few roads between the Mediterranean and Switzerland that allow traffic to flow towards Italy. Anticipating a landing of the allies in Provence, the German army considered withdrawal through Italy; it was thus necessary to maintain these communication and transport routes open and under control. In addition to an access road, it was essential for the Germans to ensure the transportation of aluminum and magnesium stocks from the "Lower Romansh" plants to Germany.
Topographically the GBMZ is characterised by granitic low relief areas with former volcanoes forming -high hills. Several plate tectonic reconstructions propose an Archean-Paleoproterozoic connection between the cratonic core of North America, the continent Laurentia, and that of Siberia, the continent Siberia, based on geological connections and paleomagnetic evidence. For example, in the reconstruction of Angara in Siberia matches the Wopmay orogen and the GBMZ in Laurentia; and the Aktikan fold belt in Siberia matches the Thelon-Taltson belt in Laurentia. Several other tectonic models have been proposed, however, and the possible connections between the two early continents remain controversial.
The market and stift were walled in and a moat was built. In 1252 Einbeck received a town charter and a town council was established. In 1279 the town received through its sovereign, Heinrich Mirabilis, an extension of its town charter. Einbeck was topographically extended and a town wall is mentioned that enclosed the market church St. Jacob and the stift St. Alexandri. St Jacob was (and is) located in the center of the city around the ‘old market’, St. Alexandri was built only some hundred meters away. Extensions were called the ‘new market’, first mentioned 1389 as was the ‘new town’.
Transform faults are plate boundaries, meaning that on either side of the fault is a different plate. In contrast, outside of the ridge-ridge transform fault, the crust on both sides belongs to the same plate, and there is no relative motion along the junction. The fracture zone is thus the junction between oceanic crustal regions of different ages. Because younger crust is generally higher due to increased thermal buoyancy, the fracture zone is characterized by an offset in elevation with an intervening canyon that may be topographically distinct for hundreds or thousands of kilometers on the sea floor.
The account of Muir visiting Mt. San Jacinto appeared first in Frederick, K. P. (1926) Legends and History of the San Jacinto Mountains. Long Beach, CA. San Jacinto Peak is one of the most topographically prominent peaks in the United States, and is ranked the sixth most prominent peak in the 48 contiguous states. According to John W. Robinson and Bruce D. Risher, authors of The San Jacintos, "No Southern California hiker worth his salt would miss climbing 'San Jack' at least once." Known for its spectacular north escarpment, the peak rises over above San Gorgonio Pass.
Norwood, also known as Bainbridge, is a working-class residential neighborhood in the northwest Bronx, New York City. It is bounded by Van Cortlandt Park and Woodlawn Cemetery to the north, the Bronx River to the east, and Mosholu Parkway to the southwest. The area is dominated topographically by what was once known as Valentine's Hill, the highest point being near the intersection of 210th Street and Bainbridge Avenue, where Gun Hill Road intersects, and around the Montefiore Medical Center, the largest landowner and employer of the neighborhood. Norwood's main commercial arteries are Gun Hill Road, Jerome Avenue, Webster Avenue, and Bainbridge Avenue.
The border starts in the west at the tripoint with Myanmar on the Mekong river, proceeding southwards via a series of irregular overland lines. The border then turns sharply eastward and continues overland, before turning sharply northward, continuing in that direction for some distance, before again turning eastward and terminating at the Vietnamese tripoint at the Shiceng Dashan peak.China, Vietnam and Laos Sign the Treaty on Definition of the Tri-Junction Point of the National Boundaries The border on both sides is predominantly inhabited by minority people groups. Topographically it is mountainous and forested, with some limited agriculture.
In the evening of 22 October, Vardar Army gathered in the valley of Pčinja River. While Zeki Pasha had the precise information about the strength and disposal of the Serbian forces, the Serbian command did not realise that the battle with the main Ottoman force would start the very next morning. Not expecting the attack, Serbs did not fortify their positions, which were topographically strong. Still, only two out of five infantry divisions were deployed in the front echelon – Danube Division I on the left wing, with Cavalry Division behind it, and Morava Division I on the right wing.
The suggestion for these files came from Luria Ben-Zion, an historian from the Hebrew University of Jerusalem, who wrote in 1940 to the Jewish National Fund (JNF) that "This would greatly help the redemption of the land". Yossef Weitz, the head of the JNF settlement department immediately suggested that they be turned into a "national project". Yitzhak Ben-Zvi suggested that, apart from topographically recording the layout of the villages, the project should also include exposing the "Hebraic origins" of each village. According to Ilan Pappé, in the early 1940s, topographers, (aerial) photographers and Orientalists worked on the files.
Senecio keniensis makes its home mostly in the lower alpine or moorland zone located at altitudes of to that can be characterized by high soil moisture, a thick humus layer, similar terrain, and not a lot of different species present. The upper alpine zone, to , is more topographically diverse, and contains a more varied flora, including the giant rosette plants Lobelia telekii and L. keniensis, Senecio keniodendron and Carduus spp.. S. keniensis can be found in both the lower and upper alpine zone, although it is less common above where it can regularly hybridise with S. keniodendron.
Finally, in locating institutional buildings, Geddes plan for Tel Aviv called for "the spatial concentration of cultural institutions" to be located prominently and in close proximity so as to both "prevent their mutual forgetfulness"Geddes cited by Meller, H. Patrick Geddes social evolutionist and city planner,. 1990, p. 280. and to provide cultural expression. Topographically the Habima theatre area was already sited for this purpose but its location at the north-eastern edge prevented it from stitching together the old and new cityWelter, Volker M. The 1925 Master Plan for Tel-Aviv by Patrick Geddes, Israel Studies vol.
In the north and east of Santa Cruz Department the crystalline and Precambrian Guaporé Shield (also called Central Brazil Shield) makes up most of the bedrock but is mostly covered by Tertiary laterites and Quaternary alluvial basins.METALLIFEROUS ORE DEPOSITS OF BOLIVIA The shield expresses itself topographically as a large elevated hinterland located north of Serranías Chiquitanas towards the Brazilian border. High-grade metamorphic rocks occur in the Bolivian part of the Guaporé Shield partly due to the 2000 million years old "Trans-Amazonian tectonothermal event" that affected parts of South America. Low-grade metamorphic rocks occur as well.
Topographically, the inside this boundary is a bowl through which the creek flows, formed by ridges and plateaus of as high as in elevation, and breached by valleys of the Webutuck's tributaries in the area, and the Webutuck itself at the north end, near the lake. The station area that gave the district its name lies at the low point, around . Most of the land is used for agricultural purposes, as fields or pasture, with some areas remaining as woodlots. Because of the clearing, it offers scenic views in every direction, particularly of the Taconic Mountains to the north and east.
Satellite rings and gaps in the rings are named for scientists who have studied these features; drawings that show these names are also included in the pertinent Transactions volume. Names for atmospheric features are informal at present; a formal system will be chosen in the future. The boundaries of many large features (such as terrae, regiones, planitiae and plana) are not topographically or geomorphically distinct; the coordinates of these features are identified from an arbitrarily chosen center point. Boundaries (and thus coordinates) may be determined more accurately from geochemical and geophysical data obtained by future missions.
Although a piece of local folklore once suggested that it came from a wrecked Spanish Armada ship, it appears that the Herdwick was an important breed in the Lake District by the end of the 12th century. For centuries, the husbandry of Herdwick sheep has been a large factor in shaping the culture and terrain of the Lake District. Topographically, grazing by sheep continues to keep the hillsides of fells largely treeless, and the ubiquitous dry stone walls of the valleys were built to protect grazing land and to confine livestock. Linguistically, many words of Lakeland speech relate to sheep husbandry.
Lake Bassano was a proglacial lake that formed in the Late Pleistocene during the deglaciation of south-central Alberta by the impoundment of a re- established drainage system and addition of glacial meltwater. It is associated with the development of through-flowing drainage within the Red Deer River basin in particular, and the South Saskatchewan drainage network in general. Approximately 7,500 square kilometers of the Bassano basin is covered with lacustrine sediments. These sediments are bordered by the topographically higher Buffalo Lake Moraine to the west, the Suffield Moraine to the east and the Lethbridge Moraine to the south.
The plains also embay the Caloris Formation and account in particular for the skeletal map pattern of the Van Eyck Formation. The ubiquitous distribution of smooth plains in topographically low regions supports the hypothesis that these materials were deposited in a fluid or semifluid state as basin ejecta or volcanic flows. The plains are thought to be slightly younger but dose to the same age as the Caloris Basin materials; thus parts of the plains are probably Caloris ejecta, either impact melt or very fluid debris flows. No obvious secondary craters from Caloris have been recognized on the smooth plains.
Mesoscale meteorology is the study of atmospheric phenomena that has horizontal scales ranging from 1 km to 1000 km and a vertical scale that starts at the Earth's surface and includes the atmospheric boundary layer, troposphere, tropopause, and the lower section of the stratosphere. Mesoscale timescales last from less than a day to weeks. The events typically of interest are thunderstorms, squall lines, fronts, precipitation bands in tropical and extratropical cyclones, and topographically generated weather systems such as mountain waves and sea and land breezes.Online Glossary of Meteorology, American Meteorological Society , 2nd Ed., 2000, Allen Press.
Only on the east, between the headwaters of the Greta and Caldew, does a bridge of higher ground strike out to connect with the rest of Lakeland, a long ridge curving southward to connect with Great Mell Fell in the Eastern Fells. This ridge, whilst significant topographically, is in many places unnoticed on the ground. The deep trough of Bassenthwaite wards off the North Western Fells, while the Central Fells rise beyond Keswick and the Greta. North of the area defined by Wainwright the countryside takes on a moorland character, gradually declining toward the Solway Firth.
Topographically, plasma treatment changes the surface morphology, with different morphologies resulting from different plasma gases used. Contact angle decreased with treatment by some, but not all, plasma gases – in one study, argon plasma decreased the contact angle from about 105 degrees to 30 degrees after 1 hour of treatment, but oxygen plasma did not affect the contact angle. Surface energy increased from 16.4 mN/m to 48.8 mN/m after ammonia plasma treatment and 36.8 mN/m after hydrogen plasma. The aluminum stud pull-off test showed an increase from 31 N to about 200 N after either ammonia or hydrogen plasma treatment.
In many regions, the forest industry is of major ecological, economic, and social importance, with the United States producing more timber than any other country in the world. Third-party certification systems that provide independent verification of sound forest stewardship and sustainable forestry have become commonplace in many areas since the 1990s. These certification systems developed as a response to criticism of some forestry practices, particularly deforestation in less-developed regions along with concerns over resource management in the developed world. In topographically severe forested terrain, proper forestry is important for the prevention or minimization of serious soil erosion or even landslides.
Alba Mons is so large and topographically distinct that it can almost be treated as an entire volcanic province unto itself. The oldest part of the northern rise consists of a broad topographic ridge that corresponds to the highly fractured terrain of Ceraunius Fossae. The ridge is oriented north-south and forms part of the Noachian-aged basement on which Alba Mons sits. Also located in the northern rise are lava flows of the Ceraunius Fossae Formation, which are somewhat older than the Amazonian- aged flows that make up much of the central Tharsis region to the south.
The route to Eilat crosses hundreds of kilometers of rough desert terrain, with frequent elevation changes and the potential for flash floods. This is particularly challenging to high-speed railway construction whose aim is avoid sharp curves along the route. The topographically challenging nature of the route (and consequently the large investment required) is one of the main reasons the railway hasn't been constructed to date, despite the frequently expressed desire of various Israeli governments for such a line to be built. The railway's proposed route can be divided into three parts: Beersheba–Dimona, Dimona – Mount Tzin and Mount Tzin – Eilat.
This includes the 365 million year old Chagrin Shale, the 360 million year old Cleveland Shale, the 358.9 million year old Bedford Formation, the 360 million year old Berea Sandstone, and the 354.8 to 351.4 million year old Orangeville Shale of the Cuyahoga Formation. The Berea Sandstone is highly resistant to erosion, and the highest waterfalls on Euclid Creek occur where the stream has cut down to the Berea. Topographically, the underlying geology creates three distinct areas: The Allegheny Plateau, the Portage Escarpment, and the Erie Plain. The headwaters of both the main and east branch are located on the Allegheny Plateau.
Serpentine outcrops in the Siskiyou Wilderness foster the growth of Jeffrey pine For the majority of the route, the Bigfoot Trail is in the Klamath Mountains. Topographically, the Klamath Mountains are part of the set of coastal ranges that run roughly parallel to the Pacific Ocean in California and Oregon, but the Klamath Mountains differ in history, complexity, and geological character. In fact, the Klamath Mountains' closest geological connection is to the Sierra Nevada (U.S.). While most of northwest California can geologically be referred to as the Klamath Mountain Province, the region also presents a coastal area called the North California Coast Range.
The Chittagong Hill Tracts in Bangladesh The Chittagong Hill Tracts (), often shortened to simply the Hill Tracts and abbreviated to CHT, are group of districts within the Chittagong Division in southeastern Bangladesh, bordering India and Myanmar (Burma). Covering , they formed a single district until 1984, when they were divided into three districts: Khagrachari District, Rangamati Hill District, and Bandarban District. Topographically, the Hill Tracts are the only extensively hilly area in Bangladesh. It was historically settled by many tribal refugees from Burma Arakan in 16th century and now it is settled by indigenous peoples who have been living there since.
Saint Anthony Hall is located on Gallows Hill, topographically the highest elevation Hartford, just north of the Trinity College campus, on the corner of Summit Avenue and Allen Place. It is a two-story French Gothic Revival building finished with a facade made of quarried New Hampshire granite laid in random courses. Externally, it appears to be rectangular structure with a rounded apse at one end and a steeply pitched hip roof. Prominent features include round towers, one tall and the other short, at two corners of the building, each topped by a conical roof with flared eave.
"However there is one very basic difference," writes Weitzmann, "in Cotton Genesis the corn is deposited in granaries that have the shape of beehives, the traditional form of an Egyptian granary, whereas in San Marco the granaries are depicted in the shape of pyramids, of which three in front might suggest a knowledge of the pyramids of Gizeh." An identical image of the pyramids does appear in Cotton Genesis in a different scene, "Joseph Selling Corn," where "they are not meant to be granaries but form the background to indicate, topographically, that this scene takes place in Egypt."Weitzmann 1984, 137.
Two morainic complexes have been recognized in the Cordillera de Mérida: one between 2,600 and 2,800 m altitude, and another one between 2,900 and 3,500 m. These two levels have been considered as Early and Late Stades, respectively, of the Mérida Glaciation. The moraines of the Late Stade are topographically well represented, and several superposed moraines, or morainic complexes, are found. The glaciated area in Cordillera de Mérida during the Last Glacial Maximum was approximately 600 km2 In the Sierra de Perija, the existence of moraines has been mentioned at altitudes between 2,700 and 3,100 m.
The loop was originally proposed as a part of a model of the basal ganglia called the parallel processing model, which has been criticized and modified into another model called the center surround model. Current organization schemes characterize cortico-basal ganglia interactions as segregated parallel processing, meaning there is little convergence of distinct cortical areas in the basal ganglia. This is thought to explain the topographically organized functionality of the striatum. The striatum is organized on a rostro-caudal axis, with the rostral putamen and caudate serving associative and cognitive functions and the caudal areas serving sensorimotor function.
Topographic map of the Bighorn Basin (highlighted in orange), formed by the Laramide Orogeny In the United States, these distinctive intermontane basins occur principally in the central Rocky Mountains from Colorado and Utah (Uinta Basin) to Montana and are best developed in Wyoming, with the Bighorn, Powder River, and Wind River being the largest. Topographically, the basin floors resemble the surface of the western Great Plains, except for vistas of surrounding mountains. At most boundaries, Paleozoic through Paleogene units dip steeply into the basins off uplifted blocks cored by Precambrian rocks. The eroded steeply dipping units form hogbacks and flatirons.
Makhtesh Ramon The Negev Desert comprises approximately , more than half of Israel's total land area. Geographically it is an extension of the Sinai Desert, forming a rough triangle with its base in the north near Beersheba, the Dead Sea, and the southern Judean Mountains, and it has its apex in the southern tip of the country at Eilat. Topographically, it parallels the other regions of the country, with lowlands in the west, hills in the central portion, and the Arava valley as its eastern border. Unique to the Negev region are the craterlike makhteshim cirques; Makhtesh Ramon, Makhtesh Gadol and Makhtesh Katan.
The Franconian Keuper-Lias Plains are bounded to the north and west by the muschelkalk Gäu landscapes of the Main-Franconian Plateaux, to the southwest, of which, are the Gäu Plateaus. In the southwest, are the geologically and topographically similar Swabian Keuper-Lias Plains. To the east, the landscape transitions into the Malm Plateau of the Franconian Jura, to the northeast are the Upper Palatine-Upper Main Hills (especially the Upper Main Hills) as a buffer zone between the Franconian Jura and the Upper Palatine-Bavarian Forest. The conurbation of Nuremberg, with its outlying towns of Fürth and Erlangen, lie roughly in the centre of the Franconian Keuper-Lias Plains.
However, Cao Cao had set his sights on a concentrated confrontation at the topographically advantageous city of Guandu (官渡; northeast of present-day Zhongmu County, Henan) to the south, thus the purpose of defending Boma might only be to delay enemy advances across the river. Cao Cao also placed Yu Jin at the nearby Yan Ford (延津; north of present-day Yanjin County, Henan) with 2,000 troops and went back to the capital at Xu City to make further battle preparations. He returned to his battle command at Guandu after putting down Liu Bei's rebellion in Xu Province sometime between February 3 and March 2, 200.
The city is located 20 to 30 km north of central Tokyo, roughly at the center of the Kantō Plain. Situated in the southeast of Saitama Prefecture, the city is topographically comprised by lowlands and plateaus, at mostly less than 20 m above sea level, with no mountain ranges or hills within the city boundaries. The western portion of the city lies on the lowland created by the Arakawa River along with those created by small rivers such as the Moto-Arakawa River, Shiba River, and Ayase River. The rest of the area mostly resides on the Ōmiya Plateau lying in the north-south direction.
The Sycamore wood lies in the north-west corner of the park and is topographically the highest point in the park. The site would have been categorised as ancient woodland until the end of the 19th century when it was felled and replanted with sycamore trees, to provide fuel for the house's biomass burners. They too were left unmanaged when the house was abandoned and have grown too tall and too close together. The modern management of this area is therefore to thin out the sycamore and add in native broadleaf trees (oak, hazel, birch and beech) to improve the health and biodiversity of the woodland.
The authoritative The Victoria history of the county of Stafford: Volume 8 (1965) suggest the origins of the name - that it arises from the British pencet ('end or head of the wood') and the Old English hyll (hill). Ward (1843)John Ward. The Borough of Stoke-upon-Trent (1843) also mentioned the possibility of the use of the Celtic British Pen (head) and Kyl (kiln). The idea of a 'head' or 'end' is topographically apt, since the village is sited on the elevated end of a long strip of valley-side woodland which begins at the ancient Bradwell Wood five miles to the north.
Topographically, the Sangamon River State Fish and Wildlife Area is a patch of central Illinois bluffland characterized by loamy hills and ravines on the bank of the Sangamon River. The trees are mostly oak and hickory, with a ribbon of bottomland softwoods, such as sycamore, along the river bank. Hunters use this public land to hunt coyote, deer, fox, mourning dove, quail, rabbit, raccoon, squirrel, turkey, and woodcock. As of 2012, the Sangamon River State Fish and Wildlife Area is managed from nearby Chandlerville as a disjunct area of the Jim Edgar Panther Creek State Fish and Wildlife Area by its owner, the Illinois Department of Natural Resources.
Topographically it transitions to the Vorberge almost seamlessly. Within and on the edge of the Sieben Berge rise several brooks whose waters flow, sooner or later, into the Leine. There are no roads through the unpopulated Sieben Berge, but it is crossed by several forest tracks and walking trails (including the roughly 15 km long Snow White Path, which was named in 2002), on which the wooded terrain can be explored. It may be reached via, for example, the winding state road (Landesstraße) of the L 485 which branches off the B 3 in Alfeld, and which runs northeast linking Alfeld with Sibbesse and, further to the north, Hildesheim.
The climate of Seoul features a humid continental climate with dry winter, called "Dwa" in the Köppen climate classification. Seoul is classed as having a temperate climate with four distinct seasons, but temperature differences between the hottest part of summer and the depths of winter are extreme. In summer the influence of the North Pacific high-pressure system brings hot, humid weather with temperatures soaring as high as 35 °C (95 °F) on occasion. In winter the city is topographically influenced by expanding Siberian High- pressure zones and prevailing west winds, temperatures dropping almost as low as -20 °C (-4 °F) in severe cold waves.
This occurred at deeper levels, at the intersection with the groundwater table (forming groundwater silcrete), or close to the surface, within the soil profile (forming pedogenic silcrete). Groundwater silcretes typically formed in more localised, topographically lower settings such as valley bottoms and slopes, whereas pedogenic silcrete tended to form extensive sheets over very large areas. Over long periods of time, as the landscape was lowered further by weathering and erosion, the silcrete became exposed at the surface as a lag gravel, an armoured carapace of gibbers (also known as a desert pavement), protecting the weaker regolith below from mechanical erosion. The resulting landscapes are relatively flat, undulating plains with low relief.
The geology of Zuffenhausen is, by the nature of a cuesta landscape, determined by a topographically varied picture of the different layers of rock and sediment as they were deposited in the 240 to 145 million year span of time that Zuffenhausen was part of the bottom of a tropical ocean. This is manifested in the presence of countless quarries and the many fossil discoveries from a layer of Muschelkalk at the bottom of this formation, that surfaces on several locations. On top are layers of Lettenkeuper and Gipskeuper that indicate the area's height around sea level at the time of the Triassic period.Gühring/Kull, pp.
The name Villarbasse (until the 19th century Villar di Basse or in Latin Villaro Bassiorum) is composed of Villar, indicating in Piedmont and in the Occitan area a sparse settlement and the determinative Basse, indicating in northern Italy, topographically depressed areas, often with stagnation of water. [Gianmario Raimondi – La toponomastica – Elementi di metodo. Stampatori, 2003.] The nucleus of the town is divided into Palassoglio (“Little Palace”, under the jurisdiction of the commendatory abbots of San Solutore and Carré (“Quadrated”, under the jurisdiction of the lay feudatories). The hamlets of Corbiglia (Curtis Vetula, “Old Manor”) and Roncaglia were once indicated as "Villar di Mezzo" (Halfway Hamlets).
According to the Appalachian Trail Conservancy, New Hampshire has the more trail above tree- line than any other Appalachian State. For northbound thru-hikers, it is the beginning of the main challenges that go beyond enduring distance and time: in New Hampshire and Maine, rough or steep ground are more frequent and alpine conditions are found near summits and along ridges. The trail reaches 17 of the 48 four-thousand footers of New Hampshire, including Mount Washington, the highest point of the AT north of Tennessee and most topographically prominent peak in eastern North America. The trail passes within half a mile of 7 additional 4000-footer peaks in the Whites.
In addition to the tuff blocks, some sections of the structure incorporated a deep fossa, or a ditch, in front of the wall, as a means to effectively heighten the wall. This second itteration of the wall containing Grotta Oscura tuff is dated by Livy to have been completed in 378 BC. Along part of the topographically weaker Northern perimeter was an agger, a defensive ramp of earth that was built up along the inside of the Servian Wall. This effectively thickened the wall and also gave the defenders of Rome a base to stand while repelling an attack. The wall was also outfitted with defensive war engines, including catapults.
Topographically, the county is dominated by mountainous and high terrain, with a great variety of natural features including valleys, canyons, gorges, rivers, glacial lakes and dense forests. Various mountains ranging between meters above sea level run the length of the county from north to south, including the Korab mountains in the east with Mali i Gramës and Korab at an altitude of being the highest mountain in the county and as well as in Albania. The Dejë mountain rises in the center, while in the east the county is dominatet by the Lura mountains. The Skanderbeg mountains on the west separates the Central Mountain Range with the Western Lowlands.
The lower valleys of Idamalayar and Pooyamkutty Ar constitute the Lower Periyar Valleys. The exceedingly violent impact of very heavy rainfall on a likely geologically unstable part of the Western Ghats where there is extensive faulting has caused accelerated weathering and erosion, carving out a complex of deep valleys on the western face of the High Range Plateau. This topographically complex segment of the Western Ghats extends from near Neriamangalam in the southwest to Panamkutty in the southeast along the Periyar River and continues north up to the watershed divide between the Periyar and the Chalakudy Basins. Its eastern border is the main Anamalai ridge.
At (53.5921°, −2.0385°) and north-northwest of London, Denshaw stands about above sea level, northeast of Manchester city centre, on elevated Pennine ground by the River Tame, which flows southwesterly from its source near the Dowry and New Year's Bridge reservoirs. The land-use of Denshaw, which centres on a road junction, is predominantly residential, the outlying land being a mixture of permanent grassland and heath. Denshaw lies amongst the South Pennines, and is topographically characterised by hilly, upland terrain. Denshaw is not contiguous with any other settlement and for purposes of the Office for National Statistics, does not form part of the Greater Manchester Urban Area.
The Galbreath Wildlands Preserve lies in the upper Navarro Watershed in the Coast Range of northern California. Located approximately inland from the Pacific Ocean in southern Mendocino County, this topographically diverse landscape ranges from 900 to 2,200 feet (275 to 670 meters) in elevation and includes coniferous forests (Douglas-fir and redwood), mixed hardwood-conifer forests (Douglas-fir, tanoak, madrone), oak woodlands (mostly black and Oregon white oaks), and annual grasslands and riparian woodland. Rancheria Creek flows northward through the preserve, along with numerous seasonal tributaries, and drains into the Navarro River. The nearest towns are Cloverdale (20 miles/32 km) and Boonville (18 miles/29 km).
According to the U.S. Census Bureau, the county has a total area of , of which is land and (0.5%) is water. A large county, roughly 1/3 of its area is tribal land, 1/3 is federal land (administered by the National Park Service, the United States Forest Service and the Bureau of Land Management), and 1/3 private or state/county land. It is also varied topographically, ranging in elevation from about to more than , and from high Colorado Plateau desert to alpine tundra. The county has the second largest reservoir in Colorado, McPhee Reservoir, many other large reservoirs, and hundreds of private lakes and ponds.
Howell Mountains was ultimately applied as well to the peaks to the south that separate Napa Valley from Suisun Valley. For example, Kunkel and Upson (1960) identify the Howell Mountains in their report on the geology and water resources of Napa County, and it is used similarly in other agricultural and geological publications, as well as by the wine industry, and in Napa County and Solano County reports. Because these mountains are not officially named, they are sometimes referred to as either the Mayacamas or Vaca Mountains, which leads to confusion as the Howell Mountains for much of their extent are topographically and geologically distinct from adjacent ranges.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (0.04%) is water. While only the third largest county by area in the state of Nevada, it is the seventh-largest county in area in the United States, not including boroughs and census areas in Alaska. The south cliff of Mount Rummel, the summit of which is just north of the county line in by this places side: White Pine County, contains the highest point in Lincoln County at . The highest independent mountain completely within Lincoln County is Shingle Peak, while the county's most topographically prominent peak is Mormon Peak.
View of Breitenthal in the wintertime Breitenthal lies in a zone characterized mainly by an oceanic climate with a prevailing wind direction from southwest to northwest. The topographically favourable location of the municipality's main centre in a hollow sloping gently towards the east confers a somewhat more favourable climate than that which prevails in nearby places. Very seldom is there hot and humid weather here. Because Breitenthal lies alee of the Wildenburg mountain ridge to the west and the Idar Forest to the north, showers and storms, as well as mean and absolute wind speed, are significantly less intense than would be expected given the synoptic structure.
As van Alsloot's works are generally topographically accurate, it is possible to identify places that still survive, especially near the abbeys of Groenendael and Ter Kameren. His series of views of the abbeys in the Sonian Forest was presumably made on commission for the Archduke Albert. He painted several versions of the winter view of Groenendael, all with differences as well as a few summer views.Denis van Alsloot, A View of the Abbey of Groenendael Near Brussels in Winter at Sotheby’s Paradise with the Four Elements, with Hendrick de Clerck Some of his works have an archaic feeling and appear inspired by landscape painting of the 16th century.
Regarding how distant the station is from downtown, its official name, Belgrade Center, is often mocked and ignored by the citizens and passengers who almost without exception call it Prokop. Member of the Serbian Academy of Sciences and Arts and a public transportation expert, Vukan Vučić, labeled Prokop as the "most disastrous error of the Belgrade transportation". He asserted that Prokop, in functional terms, is not a station at all and that, though it has been named Belgrade Centre, is actually further from the city's centre than the old station was. He added that the location is a neglected, desperately bad choice and topographically inaccessible from all sides.
He made in 1609 a topographically useful and at the same time artistically valuable view of the city of Vienna. Around the same time, he was in Vienna one of the contributors to a painted scientific work known as the "Museum or bestiary (Tierbuch) of Emperor Rudolf II", which consists of 180 parchment leaves and is kept in the Austrian National Library as cod. min. 129-130.Thomas DaCosta Kaufmann, Arcimboldo: Visual Jokes, Natural History, and Still-Life Painting, University of Chicago Press, 2009, p. 125 Two collaborations on small cabinet miniatures between father and son Hoefnagel are known, Diana and Actaeon (Louvre) and Allegory on Life and Death (British Museum).
This is analogous to air flowing rapidly out of a balloon when the neck of the balloon is left open. The air in the balloon has a higher pressure than the surrounding air so the air flows out of the balloon until the pressure inside and outside of the balloon is equal. If Central America were topographically flat, the air would flow uninterrupted from the Caribbean to the Pacific Ocean; however, the Cordillera mountains, which run along the west coast of Central America, block this flow. As a result, the air is funneled into a narrow mountain pass near Lake Nicaragua and the Gulf of Papagayo, creating the Papagayo jet.
Drawing from Ladhe's "stambog" Lahde's "stambog" I-II, now kept in the Royal Danish Library, is a sort of guestbook which he notebooks he had with him on travels where people he met could write or make drawings. Most of the texts, drawings and gouachernes are by young artists from the Art Academy, most of them unknown today but the two books contain drawings by F. Camradt, C. D. Fritsch, Hans Hansen, Johan Ludwig Lund, Elias Meyer, C. F. Stanley, Runge, Friedrich, Bertel Thorvaldsen and C. W. Eckersberg. Most of the drawings are of imaginary landscapes but some are of topographically identifiable scenes or portraits.
Allostery is the most direct and efficient way for regulation of biological macromolecule function induced by the binding of a ligand at an allosteric site topographically distinct from the orthosteric site. Due to the inherent high receptor selectivity and lower target-based toxicity, it is also expected to play a more positive role in drug discovery and bioengineering, leading to rapid growth on allosteric findings. Allosteric Database (ASD) provides a central resource for the display, search and analysis of the structure, function and related annotation for allosteric molecules. Currently, ASD contains allosteric proteins from more than 100 species and modulators in three categories (activators, inhibitors, and regulators).
The shorter, newer southern rift zone consists of a topographically plunging rift, surrounding by subtle, discontinuous faults. Camera tows along the southern flank reveal that the area is built of delineated sheet flows, small lava ponds, and lava channels. The youngest of the flows on Axial Seamount are aligned along the two rift zones, followed by flows inside the summit caldera; the oldest appear to originate from directly around the caldera, where most of the basalt is completely covered in accumulated sediment. This suggests a bilateral growth pattern, a trend also found in Hawaiian volcanics and other well-known seamounts, for instance Jasper Seamount.
The Sackwald lies on the eastern edge of the Leine Uplands in the Lower Saxon Hills. It is located between the town of Alfeld on the River Leine to the northwest and the rather more distant town of Bad Gandersheim to the southeast. The Sackwald is surrounded by the ridges of the Vorberge to the north, the southeastern foothills of the Hildesheim Forest to the north-northeast, the Sauberge to the northeast, the Harplage to the east-northeast, the Heber to the east, the Helleberg to the south and southwest, the Selter (on the other side of the Leine valley) to the southwest and the Sieben Berge to the northwest. Topographically it transitions into the last-named ridge seamlessly.
After the collapse of the Roman Empire (5th century AD), lack of maintenance of the irrigation systems associated with a cooling climate phase (i.e. the so-called Migration Period or The Dark Age Cold Period) led to the progressive waterlogging of the Po Valley and the natural depressions on the right side of the Po River turned in vast swamp basins. The waterlogging process of the area continued until the 10th century influencing the human sustenance and settling practices. According to historical-archaeological data, indeed, the wetlands were exploited for fishing as well as for transport by boat while the early medieval sites settled on the fluvial ridges, in topographically higher and strategic position in the surrounding swampy meadows.
It is the largest subregion of Asia by area, but is also the least populated, with an approximate total population of only 33 million people or 0.74% of Asia's population. North Asia is solely administrated by the Russian Federation, and makes up more than 75% of the territory of the country, but only 22% of its population, at a density of 2.5 people per km2 (6.5 per sq mi). The region of Western Siberia and occasionally Kazakhstan is usually called Northwestern Asia or Northwest Asia (), although the name sometimes refers to Caucasus or nearby provinces. Topographically, the region is dominated by the Eurasian Plate, except for its eastern part, which lies on the North American, Amurian and Okhotsk Plates.
The flow initially produces an approximately hemispherical cavity that continues to grow, eventually producing a paraboloid (bowl-shaped) crater in which the centre has been pushed down, a significant volume of material has been ejected, and a topographically elevated crater rim has been pushed up. When this cavity has reached its maximum size, it is called the transient cavity. Herschel Crater on Saturn's moon Mimas The depth of the transient cavity is typically a quarter to a third of its diameter. Ejecta thrown out of the crater do not include material excavated from the full depth of the transient cavity; typically the depth of maximum excavation is only about a third of the total depth.
Since the formation of the Black Forest and its foothills during the geological upheavals of the Upper Rhine Graben, the Wiese has shaped the landscapes in the Southern Black Forest and the Dinkelberg through its continuous erosion and sedimentation work. The Wiese flows through two topographically and geologically distinguishable sections, which divide the Wiesental valley into its upper reaches in the valley of the Schwarzwaldwiese between Fahl and Zell, and the Lower Wiesental valley in its lower reaches between Hausen and Kleinhüningen. In recent earth history, the alternation of warm and cold periods during the Pleistocene has characterized the appearance of the Wiesental. The valley of the Schwarzwaldwiese was formed by the Feldberg Glacier.
White Mountain Peak (or simply White Mountain), at , is the highest peak in the White Mountains of California, the highest peak in Mono County, and the third highest peak in the state after Mount Whitney and Mount Williamson. It is the fourteenth most topographically prominent peak in the contiguous United States. White Mountain Peak is one of only two fourteeners (peaks above 14,000 feet) in California that are not in the Sierra Nevada, the other being Mount Shasta at the far northern end of the state in the Cascade Range. It is the only fourteener in the contiguous United States that is not in the Rocky Mountains, the Cascade Range, or the Sierra Nevada.
Most of the sources Taylor cites here come ultimately from Chiang's diaries, but he also utilizes the scholarship of historian Yang Tienshi and the journalist Iris Chang. They argued that the Chinese Army needed more time to recover from its losses at Shanghai, and pointed out that Nanking was highly indefensible topographically. The mostly gently sloping terrain in front of Nanking would make it easy for the attackers to advance on the city, while the Yangtze River behind Nanking would cut off the defenders' retreat. Chinese General Tang Shengzhi Chiang, however, had become increasingly agitated over the course of the Battle of Shanghai, even angrily declaring that he would stay behind in Nanking alone and command its defense personally.
The term Brodmann area 8 refers to a cytoarchitecturally defined portion of the frontal lobe of the guenon. Located rostral to the arcuate sulcus, it was not considered by Brodmann-1909 to be topographically homologous to the intermediate frontal area 8 of the human. Distinctive features (Brodmann-1905): compared to Brodmann area 6-1909, area 8 has a diffuse but clearly present internal granular layer (IV); sublayer 3b of the external pyramidal layer (III) has densely distributed medium-sized pyramidal cells; the internal pyramidal layer (V) has larger ganglion cells densely distributed with some granule cells interspersed; the external granular layer (II) is denser and broader; cell layers are more distinct; the abundance of cells is somewhat greater.
This woreda has been topographically described as 10% highland, 30% mid-highland and 60% lowland. A rough dry-weather road 53 kilometers long connects Wegeda to the main Debre Tabor - Nefas Mewcha all-weather highway (also known as the Chinese Road).Hans Spiess, "Field Trip Report to South Gonder, North Welo and Oromiya Zones of Region 3 (Amhara) and the Southern Zone of Region 1 (Tigray)" UNDP-EUE Report (accessed 22 January 2009) Local officials announced 3 March 2009 that a number of health stations were under construction at six locations. These would join two existing health stations and 31 health posts, and provide service to over 100,000 inhabitants when they are fully operational.
En route to Katmai in 1913, Robert F. Griggs had briefly inferred landslide (debris avalanche) as the origin of Augustine's hummocky coastal topography about Burr Point, by geomorphic analogy with the hummocky and blocky deposit of a 1912 landslide near Katmai. The hummocky deposits on Augustine's lower flanks resemble both topographically and lithologically those of the great landslide or debris avalanche that initiated the spectacular May 18, 1980 eruption of Mount St. Helens. The deposit of that landslide revealed the origin of coarse diamicts with hummocky topography at other strato volcanic cones. Since 1980 many hummocky coarsely fragmental deposits on Augustine's lower flanks have come to be interpreted as deposits of numerous great landslides and debris avalanches.
In these layers the organization of the two efferent regions of the antennal lobe is represented topographically, establishing a coarse odotopic map of the antennal lobe in the region of the lip of the mushroom bodies. Mushroom bodies are known to be involved in learning and memory, particularly for smell, and thus are the subject of current intense research. In larger insects, studies suggest that mushroom bodies have other learning and memory functions, like associative memory, sensory filtering, motor control, and place memory. Research implies that mushroom bodies generally act as a sort of coincidence detector, integrating multi-modal inputs and creating novel associations, thus suggesting their role in learning and memory.
According to the 1913, Gazetteer of Surface waters, California, in San Joaquin River Basin: :"Polvadero Creek (L); Fresno County; rises in the northern part of T. 24 S., R. 15 E.; flows northeastward 18 miles into San Joaquin Valley; sinks before reaching Los Gatos Creek, to which its basin is topographically tributary; called Zapatos Creek in the upper part of its course. Fisk and Johnson map." B. D. Wood, Gazetteer of Surface waters, California, in San Joaquin River Basin, U.S. G.P.O., 1913, p.69 The Fisk and Johnson Map referred to above, is the Manuscript map of San Joaquin Valley compiled by A. J. Fisk, Jr., and H. R. Johnson, in 1866.
Idealized depiction a dryline Topographically, Oklahoma is situated between the Great Plains and the Ozark Plateau in the Gulf of Mexico watershed. The western part of the state is subjected to extended periods of drought and high winds which generates Dust storms. The eastern part of the state is humid subtropical climate zone. The Dry line, an imaginary line that separates moist air from an eastern body of water and dry desert air from the west, usually bisects the state and is arguably an important factor in pre-historic settlement, with agrarian tribes settling in the eastern part of the state and Hunter-gatherer tribes settling in the western part of the state.
However, these areas can still be included in topographically defined basins if one considers the hypothetical flow of water (or ice), and thus nutrients or pollutants, over the surface of the ground (or ice sheet); this is the approach taken here. For example, the Antarctic ice sheet can be divided into basins, and most of Libya is included in the Mediterranean Sea basin even though almost no water from the interior actually reaches the sea. Major continental divides, showing drainage into the major oceans and seas of the world--Drainage basins of the principal oceans and seas of the world. Grey areas are endorheic basins that do not drain to the ocean.
Topographically the countryside varies from the open rolling plains of the south of the Alentejo to the granite hills that border Spain in the northeast. To feed the water needs of this considerable area a number of public dams have been constructed, most notably the Alqueva Dam. The landscape is primarily one of soft rolling hills and plains, with conspicuous shrubs and the native cork oaks and holly/holm oaks, the established olive trees and grapevines, plus some large-scale toilet roll production of eucalyptus trees and some native trees. In the north, traditional economic activity may be more livestock-based as typified by cattle, sheep, and pig (both white and black) farming.
The issue that triggered the siege was alleged livestock theft in the Herschel area. In the aftermath of the siege, Phuthi people dispersed widely over what is contemporary southern Lesotho and the northern Transkei region, to escape capture by the colonial powers. It is for this reason, it has been hypothesised, that Phuthi villages (including Mpapa, Daliwe, Hlaela, Mosifa and Mafura—all to the east of Mount Moorosi, in Lesotho) are typically found in such topographically mountainous regions, accessible only with great difficulty to outsiders). After the siege of "Moorosi's rebellion", many Phuthi people were captured, and forced into building the bridge (now, the old bridge) at Aliwal North that crosses the Senqu (Orange River).
The highest peak is sometimes known as Sleeping Ute Mountain; the entire range is also identified as one large mountain, called Sleeping Ute Mountain, on some maps; and the range is sometimes called the Sleeping Ute Mountains. All of these forms of the mountain's name and of the range's name can be found on various USGS maps, databases and reports. The Ute Mountains, with a collective profile commonly known as "The Sleeping Ute", are a dense cluster of peaks approximately in extent and stand in isolation from other mountains. Despite being much lower than Colorado's highest peaks, Ute Mountain is the eighth most topographically prominent peak in the state, due to this isolation.
Medial view of the right cerebral hemisphere showing the entorhinal cortex in red at the base of the temporal lobe The dorsalcaudal medial entorhinal cortex (dMEC) contains a topographically organized map of the spatial environment made up of grid cells. This brain region thus transforms sensory input from the environment and stores it as a durable allocentric representation in the brain to be used for path integration. The entorhinal cortex contributes to the processing and integration of geometric properties and information in the environment. Lesions to this region impair the use of distal but not proximal landmarks during navigation and produces a delay- dependent deficit in spatial memory that is proportional to the length of the delay.
At (53.5166°, −2.4668°), and northwest of central London, Tyldesley is situated 7.7 miles (12.4 km) east-southeast of Wigan and 8.9 miles (14.3 km) west-northwest of the city of Manchester, and at the eastern end of the Metropolitan Borough of Wigan. Tyldesley and Shakerley cover Topographically Tyldesley is situated the edge of the Lancashire Plain just to the north of Chat Moss and the Banks of Tyldesley are where the foothills of the Pennines begin. The land rises from about at the foot of the banks to at the highest point. The banks, a sandstone escarpment with the scarp slope facing south and the gentler dip to the north, are about one and a half miles long.
Double Mountains is the name of a pair of flat-topped buttes located southwest of Aspermont in Stonewall County, Texas. While the Handbook of Texas gives their elevation as either or , United States Geological Survey maps give the elevation of the western mountain as and that of the eastern mountain as between and . Together, the mountains form part of the high ground dividing the watersheds of the Salt Fork and Double Mountain Fork Brazos River. Rising some 500–800 feet (150–250 m) above the surrounding plains, the higher eastern mountain is the highest point in Stonewall County and the most topographically prominent point for almost , the nearest more prominent peak being Mount Scott in Oklahoma.
As Parry writes, "the precedent of a classical architectural fantasy on this scale supplies an alternative to the natural assumption that the Titan's goblet was actually made by a giant who simply left it behind".Parry, 133 But a literal rendition of this image may not have suited Cole's art: being a landscape artist, he would have been more comfortable expressing it only topographically, avoiding the need to render a massive stone human form. A fantastical sketch of a fountain and basins by Cole, c. 1832–33 Cole's drawingsFound in his sketchbooks at the Detroit Institute of Arts from his trip to Europe or shortly thereafter also appear to prefigure the Goblet.
Topographically, the Golan Heights is a plateau with an average altitude of 1,000 metres, rising northwards toward Mount Hermon and sloping down to about elevation along the Yarmouk River in the south. The steeper, more rugged topography is generally limited to the northern half, including the foothills of Mount Hermon; on the south the plateau is more level. There are several small peaks on the Golan Heights, most of them volcanic cones, such as: Mount Agas (1,350 m), Mount Dov/Jebel Rous (1,529 m; northern peak 1,524 m),Yigal Kipnis, The Golan Heights: Political History, Settlement and Geography since 1949, Routledge 2013, , accessed 9 August 2019 Mount Bental (1171 m) and opposite it Mount Avital (1204 m), Mount Ram (1188 m), Tal Saki (594 m).
A typical home in Denia A Denia (; other spellings Danya, Dania, Denya) is a district of Haifa, Israel, located on Mount Carmel. Denia and its associated neighborhoods capture the southernmost part of Haifa's jurisdiction area, which is also the highest-elevated topographically, and make up the city's altogether most affluent and least densely populated residential borough, with a population count of slightly more than 11,000 in 2008.Secretary of the City of Haifa, Haifa Neighborhood Profile , June 2010, p. 327 It lies approximately 5 kilometers in a beeline from downtown Haifa (whereas twisting roads due to intervening hills and wadis make actual distance bigger) and is crossed by Aba Hushi Avenue, which has made the district sometimes be referred to as the "Aba Hushi Axis".
Piz Bernina and the Morteratsch Glacier Piz Bernina is one of the few isolated Alpine four-thousanders and the most topographically isolated mountain of Switzerland. It is the culminating point of a group of summits slightly lower than 4,000 meters (13,120 feet) mostly lying on the main watershed between Switzerland and Italy (such as Piz Scerscen, Piz Zupò, and Piz Palü). The only other summit higher than is La Spedla (the Shoulder), a minor prominence south of the mountain, which is also the highest point on the Italian side of the massif. The summit itself is located on a perpendicular chain (orientated north–south) starting at La Spedla on the border and finishing at Piz Chalchagn, composed also of Piz Morteratsch and Piz Boval.
The Fototeca Berenson contained 170,000 photographs at Berenson's death and now contains approximately 250,000 photographs. They are organized topographically, according to Berenson's original scheme: Florence, Siena, Central Italy, Northern Italy, Lombardy, Venice, Southern Italy, and within each school by artist and location. A section of the Fototeca is devoted to images of “homeless” works of art—the term used by Berenson for objects that were once on the art market but whose presents locations are now unknown. The versos of many photographs contain handwritten notes by Bernard and Mary Berenson, Nicky Mariano and other art connoisseurs from the first half of the twentieth century. A project to digitize the Fototeca Berenson, making its holdings accessible through the Harvard Libraries’ website, is currently in progress.
The section between Latrun and Jerusalem roughly follows an ancient path connecting Jaffa and Jerusalem. At the entrance to Jerusalem, the steep and winding rise was known as Ma'aleh HaRoma'im (Romans' Ascent) and covers a path rising in altitude. The Jaffa–Jerusalem road was initially made accessible for wheeled vehicles by the Ottomans in 1867Mike Rogoff, Tourist Tip #252 Sha'ar HaGai, en Route to Jerusalem, in Haaretz, 4 June 2013, retrieved 15 March 2016 and since then served as the main highway to Jerusalem, favored over more topographically convenient routes such as Route 443. The largest bell for the church of the Augusta Victoria complex, built between 1907–1910, weighed six tonnes and required that the road be widened and paved.
Mount Rainier, an active stratovolcano, is the state's highest elevation, at almost , and is the most topographically prominent mountain in the contiguous U.S. Washington is a leading lumber producer; its rugged surface is rich in stands of Douglas fir, hemlock, ponderosa pine, white pine, spruce, larch, and cedar. Washington is the nation's largest producer of apples, hops, pears, red raspberries, spearmint oil, and sweet cherries, and ranks high in the production of apricots, asparagus, dry edible peas, grapes, lentils, peppermint oil, and potatoes. Livestock and livestock products make important contributions to total farm revenue, and the commercial fishing of salmon, halibut, and bottomfish makes a significant contribution to the state's economy. Washington ranks second only to California in wine production.
Manizales has a domestic airport called La Nubia Airport which has a runway of about 1,400 meters and provides services from 6 am to 6 pm. Due to foggy weather conditions, it is often closed due to low visibility. Meanwhile, the existence of buildings over two stories close to the landing head make it topographically unfeasible to expand the airport, which in turn has become an obstacle to regional development; For these reasons, the International Coffee Airport is being built within the metropolitan area, in the town of Palestina, 25 minutes from Manizales. At an altitude of 1,525 m, the airport will have a runway of 2,800 meters which could be extended to 3,500 meters in order to receive long-range aircraft.
A drainage basin is an extent of land where water from rain and melting snow or ice drains downhill into a body of water, such as a river, lake, reservoir, estuary, wetland, sea or ocean. The drainage basin includes both the streams and rivers that convey the water as well as the land surfaces from which water drains into those channels, and is separated from adjacent basins by a drainage divide. The drainage basin acts like a funnel, collecting all the water within the area covered by the basin and channelling it into a waterway. Each drainage basin is separated topographically from adjacent basins by a geographical barrier such as a ridge, hill or mountain, which is known as a water divide.
The Twelve Bens or Twelve Pins (; the peaks of Beola) is a mountain range of mostly sharp-peaked quartzite summits and ridges located in the Connemara National Park in County Galway, in the west of Ireland. The widest definition of the range includes the Garraun Complex to the north as well as several isolated peaks to the west, and is designated a 16,163-hectare Special Area of Conservation. Topographically, the range is partnered with the Maumturks range to the east of the Inagh valley (a Western Way route); and both share a common geology being largely composed of metamorphic marine rocks, being predominantly resistant quartzite but with deposits of schists in the valleys (known as Connemara Dalradian rocks). The highest point is Benbaun at .
In the rear, reinforcements were at hand, commanded by John I of Portugal himself. In this topographically high position, the Portuguese could observe the enemy's arrival and were protected by a steep slope in their front. The rear of the Portuguese position, which was in fact its front in the final battle, was at the top of a narrow slope, which came up to a small village, and was further defended by a complex series of interlocking trenches and caltrops designed to surprise and trap the enemy cavalry. This trenching tactic was developed around this time and used extensively by both the English in France and the Portuguese in the rare set-piece battles of the Crisis of the Succession.
Brodmann area 23 is a subdivision of the cerebral cortex of the guenon defined on the basis of cytoarchitecture. Brodmann regarded it as topographically and cytoarchitecturally homologous to the combined ventral posterior cingulate area 23 and dorsal posterior cingulate Brodmann area 31 of the human (Brodmann-1909). Distinctive Features (Brodmann-1905): the cortex is relatively thin; smaller cells predominate; the cell density of the multiform layer (VI) is great, producing a distinct boundary with the subcortical white matter; the internal granular layer (IV) is rather well developed; the internal pyramidal layer (V) contains a dense population of round, medium-sized ganglion cells concentrated at the border with layer IV; layers V and VI are narrow with a distinct mutual boundary.
In today's settlement, the ground monument is located almost two kilometres east of the village Cigmău and two kilometres south-west of the small town of Geoagiu in the undeveloped, agriculturally used or wasteland "Cetatea uriasilor" (fortress of the giants) or "Progadie". Topographically, it lies on a high terrace on the northern bank of the Mureș, about two and a half kilometres below the confluence of the Geoagiu River. In ancient times, the fort probably had the tactical task of monitoring the valley of Mureș and the strategic function of controlling an area in which numerous Dacian fortresses had been located before the Roman occupation. Administratively it was first located in the province of Dacia superior, later in the Dacia Apulensis.
With a height of 225.8 m above sea level (NN), the Meesenkopf is topographically unspectacular for this part of the Wiehen Hills. There are much higher summits in its immediate vicinity, such as the Heidbrink, just under one kilometre away to the south, and the and better-known Reineberg, Lübbecke's local hill, which is 300 metres to the east, west of the Ronceva valley. Today the Meseberg has no particular importance for hikers, and on most maps it is not even shown. The hill can be climbed on forest tracks in around 30 minutes, although there is no established way to the summit itself, only a path that a few hikers over the years have beaten, which aids those making for the top.
For visitors to the ECB and the adjacent, publicly accessible area to the east, the quotations not only topographically mark the site of the mass crime as "inscriptions" on paths and walls, but in their arrangement follow the chronological sequence of a deportation: from the invitation to arrive at the collection point, to the departure of the trains to the collection camps in the east. Between which there were often only two to three days of immeasurable suffering for the people affected. However, the literal evidence also addresses indirect events and emotions, such as suicides in the temporal context of the deportations, reactions of the urban population or the reflection of crime in Frankfurt. Quotes from perpetrators were not included.
And Atoll is biologically and topographically representative of a vast majority of the atolls around Federated States of Micronesia (FSM). It is the most biologically diverse and undisturbed atoll in Pohnpei, Pohnpei's number one marine Area of Biological Significance (ABS) and one of the identified 24 “Priority Action Areas” in the Eco-regional Plan under the National Biodiversity Strategic Action Plan (NBSAP). With a significant lagoon area of approximately , the atoll, which is located 18.5 km south west of Pohnpei, is home to 13 species of reptiles, including the green turtle (Chelonia mydas) and hawksbill turtle (Eretmochelys imbricata), 25 bird species, seven mammals, and hundreds of other marine species. The proposal to make a Biosphere Reserve presents an opportunity to create a model of sustainability.
Mt. Vaca at an elevation is the highest summit, and the high point of Solano County, but the backbone of the range is the Blue Ridge, a prominent ridgetop that maintains an elevation of over for several miles. Where the Blue Ridge seemingly ends abruptly at Putah Creek Canyon, the mountains continue on the north side of the canyon as the Blue Ridge Range, which is topographically and geologically similar to the Vaca Mountains. Because the canyon is difficult to distinguish from most vantage points on the east side, the Vaca and Blue Ridge Mountains present what appears to be a nearly continuous ridge line that defines the west margin of the Sacramento Valley, which is the northern half of the -long Central Valley of California.
Gasherbrum III (; ), surveyed as K3a, is a summit in the Gasherbrum massif of the Baltoro Muztagh, a subrange of the Karakoram on the border between Xinjiang, China and Gilgit-Baltistan, Pakistan. It is situated between Gasherbrum II and IV. Gasherbrum III fails to meet a topographic prominence cutoff to be an independent mountain; hence it can be considered a subpeak of Gasherbrum II.Some sources use a lower cutoff value, and consider Gasherbrum III to be independent. Gasherbrum III was one of the highest unclimbed summits in the worldIn fact no summit in 1975 was both higher and more topographically prominent. up to its first ascent in 1975, by Wanda Rutkiewicz, Alison Chadwick-Onyszkiewicz, Janusz Onyszkiewicz and Krzysztof Zdzitowiecki, members of a Polish expedition.
The nearest to downtown, as well as the wealthiest in terms of average income, is Mockingbird Valley, and the two most prominent and oldest Eastern Jefferson County cities are Anchorage and Glenview. There are also two areas which are sometimes considered to be their own side of town. The area east of I-65, south of Eastern Parkway, and west of Bardstown Road is economically, culturally and topographically a buffer zone between the East and South sides, and is routinely claimed by both residents and outsiders as belonging to either side. The interior areas of the city's east and south ends are also sometimes considered by some to be their own side of town, sometimes called the "Inner East side".
The highest peaks, such as the Mount Rainier, dominate their surroundings for . The northern part of the range, north of Mount Rainier, is known as the North Cascades in the United States but is formally named the Cascade Mountains north of the Canada–United States border, reaching to the northern extremity of the Cascades at Lytton Mountain. Overall, the North Cascades and Canadian Cascades are extremely rugged; even the lesser peaks are steep and glaciated, and valleys are quite low relative to peaks and ridges, so there is great local relief. The southern part of the Canadian Cascades, particularly the Skagit Range, is geologically and topographically similar to the North Cascades, while the northern and northeastern parts are less glaciated and more plateau-like, resembling nearby areas of the Thompson Plateau.
Due to the difficult geological conditions in the Schanfigg valley, a total of 18 tunnels and 40 bridges needed to be created between 1912 and 1914 for the privately built Arosa line. Like most of the other bridges on the line, the Castielertobel Viaduct was constructed in the classical manner, and mainly of stone. However, the special site conditions dictated the inclusion of stampfbeton (unreinforced concrete compressed by stamping) in the cores of the stone pillars. In light of the spectacular, and topographically extremely difficult, rises and falls of the Castielertobel (the so-called Bärenfalle, or bear traps, which, despite being relatively close to the nearby cantonal road, were almost unknown before the Arosa line was constructed), the engineers had to resort to using fire and smoke signals to help them survey the line's route.
The first parts of the line were built at its southern end in Singen, far removed from the eponymous Gäu, by the Baden State Railways. The railway engineer Robert Gerwig, who hailed from Baden, was in the planning stages of a railway, which would cross the Black Forest from Offenburg to Singen, and which would become the Schwarzwaldbahn (Baden). At the time, a connection to Württemberg was not considered. The first part of that line, between Singen and Engen, which was topographically without real challenges, was opened for service on 6 September 1866. The extension of that section to Donaueschingen proved to be technically much more complex, and the construction of the ascending part of the line between Engen and Donaueschingen was not completed until 15 June 1868.
The Ninety East Ridge at the centre of the picture and the Chagos-Laccadive Ridge on the upper left side The Ninety East Ridge (also rendered as Ninetyeast Ridge, 90E Ridge or 90°E Ridge) is a mid-ocean ridge on the Indian Ocean floor named for its near-parallel strike along the 90th meridian at the center of the Eastern Hemisphere. It is approximately in length and can be traced topographically from the Bay of Bengal southward towards the Southeast Indian Ridge (SEIR), though the feature continues to the north where it is hidden beneath the sediments of the Bengal Fan. The ridge extends between latitudes 33°S and 17°N and has an average width of 200 km. The ridge divides the Indian Ocean into the West and East Indian Ocean.
Over the following seven years, Wolsey spent lavishly (200,000 Crowns) to build the finest palace in England at Hampton Court. Today, little of Wolsey's building work remains unchanged. The first courtyard, the Base Court,"Base" in this instance simply means "lower" in the hierarchy of courtyards; it is not topographically lower. (B on plan), was his creation, as was the second, inner gatehouse (C) which leads to the Clock Court (D) (Wolsey's seal remains visible over the entrance arch of the clock towerSpelthorne Hundred: Hampton Court Palace: architectural description, A History of the County of Middlesex, Volume 2: General; Ashford, East Bedfont with Hatton, Feltham, Hampton with Hampton Wick, Hanworth, Laleham, Littleton (1911), pp. 371–379. Retrieved 21 March 2009.) which contained his private rooms (O on plan).
The lot on which the meeting house, First Day school and cemetery are located is on the west side of Quaker Church Road, also at that point the boundary between the towns of Yorktown and Somers to its east. It is located north of Quaker Church's southern end at Saw Mill River Road (also U.S. Route 202, New York State Route 35 and New York State Route 118). This area was formerly the hamlet of Amawalk, which still lends its name not just to the meeting house but to the Amawalk Reservoir, part of the New York City water supply system, a half-mile (800 m) to the east. Topographically the area consists of small low hills with occasional narrow depressions, often filled by creeks or wetlands, in between.
Cliffs of Vixía Herbeira near Cape Ortegal, the highest (613 m) in continental Europe The interior of Galicia is a hilly landscape, composed of relatively low mountain ranges, usually below high, without sharp peaks, rising to in the eastern mountains. There are many rivers, most (though not all) running down relatively gentle slopes in narrow river valleys, though at times their courses become far more rugged, as in the canyons of the Sil river, Galicia's second most important river after the Miño. Meadows in Pambre, Palas de Rei Topographically, a remarkable feature of Galicia is the presence of many firth-like inlets along the coast, estuaries that were drowned with rising sea levels after the ice age. These are called rías and are divided into the smaller Rías Altas ("High Rías"), and the larger Rías Baixas ("Low Rías").
Musala is also the 3rd most topographically isolated major peak in Continental Europe. Musala is situated within the Rila National Park, which is noted for its rich flora, including species such as Macedonian Pine and Bulgarian Fir in the forests on its middle slopes, and fauna; it is one of the easiest places in Europe to see the wallcreeper. All major mountain ranges of Bulgaria can be seen from the top; these include Vitosha to the northwest, Sredna Gora towards the northeast, the Balkan Mountains along most of the northern horizon behind Vitosha and Sredna Gora, the Rhodope Mountains to the southeast, Pirin to the south, Osogovo and Ruy Mountain to the west, and of course, the rest of Rila. A cosmic ray station was built on the peak in 1960 with cooperation from the Hungarian Academy of Science.
Brodmann area 12 is a subdivision of the cerebral cortex of the guenon defined on the basis of cytoarchitecture. It occupies the most rostral portion of the frontal lobe. Brodmann-1909 did not regard it as homologous, either topographically or cytoarchitecturally, to rostral area 12 of the human. Distinctive features (Brodmann-1905): a quite distinct internal granular layer (IV) separates slender pyramidal cells of the external pyramidal layer (III) and the internal pyramidal layer (V); the multiform layer (VI) is expanded, contains widely dispersed spindle cells and merges gradually with the underlying cortical white matter; all cells, including the pyramidal cells of the external and internal pyramidal layers are inordinately small; the internal pyramidal layer (V) also contains spindle cells in groups of two to five located close to its border with the internal granular layer (IV).
The term Brodmann area 9 refers to a cytoarchitecturally defined portion of the frontal lobe of the guenon. Brodmann-1909 regarded it on the whole as topographically and cytoarchitecturally homologous to the granular frontal area 9 and frontopolar area 10 in the human. Distinctive features (Brodmann-1905): Unlike Brodmann area 6 (Brodmann-1909), area 9 has a distinct internal granular layer (IV); unlike Brodmann area 6 or Brodmann area 8 (Brodmann-1909), its internal pyramidal layer (V) is divisible into two sublayers, an outer layer 5a of densely distributed medium-size ganglion cells that partially merges with layer IV, and an inner, clearer, cell-poor layer 5b; the pyramidal cells of sublayer 3b of the external pyramidal layer (III) are smaller and sparser in distribution; the external granular layer (II) is narrow, with small numbers of sparsely distributed granule cells.
The view from Mount Carmel across the Coastal Plain to the Mediterranean Sea Israel's Coastal Plain (, Mishor HaḤof) is the coastal plain along Israel's Mediterranean Sea coast, extending north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous with the exception of the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by - north to south - the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south.
Topographic map of the Deccan peninsula showing the locations of major cities and towns. Hogenakal Falls, Tamil Nadu Tiruvannamalai hill, often regarded as the southern tip of Deccan plateau and the city of Tiruvannamalai is called as Gateway of Deccan plateau at Tamil Nadu Near Hampi, Karnataka Rock formations at Hyderabad, Telangana Hills of granite boulders are a common feature of the landscape on the Deccan plateau. Deccan Traps in Maharashtra The Deccan plateau is a topographically variegated region located south of the Gangetic plains-the portion lying between the Arabian Sea and the Bay of Bengal-and includes a substantial area to the north of the Satpura Range, which has popularly been regarded as the divide between northern India and the Deccan. The plateau is bounded on the east and west by the Ghats, while its northern extremity is the Vindhya Range.
Lobate scarps are the most common structural landforms in the Bach region. Almost all have convex slope profiles, rounded crests, and steep, sharply defined lobes. Three types are seen in the map region: (1) very small (<50 km long, ~100 m high), irregular scarps that commonly enclose topographically depressed areas; they are restricted to the intermediate and smooth plains units in the eastern part of the map region; (2) small (~100 km long, ~100 m high), arcuate or sinuous scarps, also confined primarily to the intermediate and smooth plains units in the eastern part of the map region; and (3) large (>100 km long, ~1 km high), broadly arcuate but locally irregular or sinuous scarps whose faces are somewhat steeper. Several of these scarps (lat 83° S., long 80°) deform craters and offset preexisting features vertically (FDS 166751).
Colombia is located at the intersection of six tectonic plates: CP - Caribbean Plate NAP - North Andes Plate SAP - South American Plate MP - Malpelo Plate CMP - Coiba microplate PMP - Panama microplate The topography of western Colombia is largely dominated by the Romeral Fault System, extending from northern Colombia into Ecuador The topographically pronounced Romeral Fault System encloses the Cauca Basin in south-central Colombia and forms the boundary between the Western and Central Ranges of the Colombian Andes The cities of Cali, situated in the valley of the Cauca River and Armenia, Pereira and Manizales in the adjacent mountainous areas are all affected by the movements of the Romeral Fault System with frequent smaller and occasional major earthquakes The megaregional Romeral Fault System represents the geological boundary between the Western and Central Ranges of the Colombian Andes.Rodríguez & Zapata, 2013, p.40 The fault system was active since the Triassic.Vinasco & Cordani, 2012, p.
Càrn nan Gobhar reaches a height of 993 metres (3258 feet) and qualifies as a Munro and a Marilyn. Somewhat confusingly there is another Càrn nan Gobhar, also a Munro with exactly the same height situated 14 kilometres to the north east on the northern side of Glen Strathfarrar. Càrn nan Gobhar is the lowest of the four Munros on the north shore of Loch Mullardoch and is rather overshadowed by them. Topographically it is quite featureless, being mainly composed of rolling grassy slopes interspersed with patches of rock and scree, though with steeper slopes on the west and east flanks. The hill's name translates from the Gaelic as “Cairn (i.e. hill) of the Goats”Irvine Butterfield, The High Mountains of Britain and Ireland p.318. Gives translation as “Cairn of the Goats“; Scottish Mountaineering Trust, The Munros. Gives translation as “Hill of the Goats“.
Topographically speaking, Agaw Awi is relatively flat and fertile, whose elevations vary from 1,800 to 3,100 m above sea level, with an average altitude of about 2,300 m. The Zone is crossed by about nine permanent rivers which drain into the Abay (or Blue Nile); other water features include two crater lakes, Zengena and Tirba, and Zimbiri marsh which is located 5 km south-west of Addis Kidam. Local forests include Dukma and Apini, which are located on either side of the town of Kidamaja, Zengena forest around Lake Zengena and Goobil forest which is on a dome-shaped hill next to Kessa. The Agaw have traditionally practised a land-management system which is well adapted to the local ecology, which enables them to sustain the fertility of the soil and minimize erosion; this area is recognized as one of the most productive in the Amhara Region.
Both paintings have in the lower left corner a legend which describe key locations in the battle scene which are each identified by a number in the painting. For the Retaking of Buda Geffels based his topographically correct view on an extremely rare print engraved by the Vienna-based engravers Johann Martin Lerch and Johann Jakob Hofmann after a drawing by the Dutch artist Justus van den Nypoort.György Rozsa, The Recapture Of Buda As A Pictorial Theme in: New Hungarian Quarterly, 1986, issue 103, pp. 163-165 For the Relief of Vienna Geffels relied on a print engraved by Johann Jakob Hofmann after a design by Justus van den Nypoort published soon after the events happened.Johann Jakob Hofmann, Justus van den Nypoort, The Relief of Vienna on 12 September 1683 at the Austrian National Library Prodigal son in wild living Two portraits of Ferdinando Carlo Gonzaga di Nevers have been attributed to Geffels.
Wadi al-Natrun is the common name for a desert valley located west of the Nile Delta, along the El Tahrir markaz, which is about 10 km west of the entrance to Sadat City on the Cairo- Alexandria Desert Road, and about 50 km from Khattabah on the Nile (Rashid Branch), and it falls below the level of the plateau surface surrounding it about 50 meters. The length of this depression ranges between 5, 55 and 60 km, while its average width is 10 km, and its deepest point reaches 24 meters below sea level. The depression is the smallest depression in the Egyptian Western Desert, with an area of about 500 km2. Therefore, it is true that it is a depression and not a valley, because the region is a closed depression that has a beginning and an end, and it has no source, estuary or tributaries, so the launch of the word "Wadi" on the depression is not topographically correct.
The shopping mall occupies the lower floors of an unusual building. The Art Deco McGraw-Hill Building, built in 1928 and a designated City of Chicago historic landmark, was demolished but its facade dismantled, cleaned, stored, and re-hung on the exterior of a new building on the same site. The Conrad Hotel, a luxury affiliate of Hilton Hotels, occupied the upper floors of the building, until it was renamed the Gwen in 2015 and operated by Starwood Hotels (The hotel opened under the Le Meridien flag and was converted in 2006.) The mall also occupies a topographically unusual site, as Michigan Avenue at this location is elevated, gently sloping back down to ground level from its bi-level bridge over the Chicago River. Furthermore, Nordstrom occupies floors one through four of a full-block building one block behind Michigan Avenue, at the southwest corner of N. Rush Street and E. Grand Avenue.
Moine Thrust belt defining the western edge of the Moine Supergroup outcrop Lewisian gneiss has been pushed along the thrust fault and now lies above younger well-bedded Cambrian quartzite, which itself lies unconformably above Lewisian gneiss The Moine Thrust Belt or Moine Thrust Zone is a linear tectonic feature in the Scottish Highlands which runs from Loch Eriboll on the north coast south-west to the Sleat peninsula on the Isle of Skye. The thrust belt consists of a series of thrust faults that branch off the Moine Thrust itself. Topographically, the belt marks a change from rugged, terraced mountains with steep sides sculptured from weathered igneous, sedimentary and metamorphic rocks in the west to an extensive landscape of rolling hills over a metamorphic rock base to the east. Mountains within the belt display complexly folded and faulted layers and the width of the main part of the zone varies up to , although it is significantly wider on Skye.
The English name of Prosperous was given when the village was founded in the late 18th century by Sir Robert Brooke. The village takes its Irish name from the townland lying to the east, Corrchoill or an Chorrchoill (meaning "the smooth forest"), anglicised variously as Corr[y]hill[s], Curr[i]hill[s] and Curryhills.Placenames Database of Ireland (see archival records) An alternative meaning is "The wood of the small round hill" 4 and this makes sense topographically as there is a low hill immediately to the east of the village. The village extends into the surrounding townlands of Ballinafagh, Killybegs, Curryhills and Downings (north, south, east and west, respectively). The town of Prosperous owes its origin to the vision and ideals of Sir Robert Brooke (1744-1811) from County Cavan. The late eighteenth century was a time of attempted industrial development in Ireland and the industry upon which Prosperous was founded in 1780 was cotton manufacturing.
These microbiotas have evolved to form mutually and beneficial relationships with their host, they are important for immune function, nutrition and human physiology and any disruption in the gut can lead to gastrointestinal dysfunction like obesity for example. Several studies have also shown that the diversity and the composition of the gut microbiota vary topographically and temporarily. This is because specific bacteria have been linked to the host’s food intake as well as the use of nutrition and energy metabolism. Any changes or modifications of the microbial landscape in the gut can lead to several complex and dynamic interactions throughout life. Additionally, the choice of the host is strongly associated with the diversification and complexity of the microbial, for instance, the study illustrates that diet high in fat increases the level of Bacteroidete and decreases the level of Firmicute in children’s gut, the study also theorized that diet quality is also related to gut size.
Furthermore, just two months prior on April 27, Mt. Aso had erupted and deposited 5.16 metric tons of ash which combined with the rain water to produce a debris flow. Topographically, the rivers in northern Kyushu tend to follow steep grades which cause them to flow rapidly downstream. Additionally the river systems in the area have larger drainage basins upstream than middle- and downstream with the Shirakawa River and Chikugo River having drainage basin ratios of 80%国土交通省河川局『白川水系河川整備計画 治水の現状と課題』PDF 2010年8月29日閲覧 and 70%『筑後川五十年史』p.4 respectively between their upstream and downstream systems. These topographical features resulted in the upstream systems quickly accumulating and transporting water in amounts that the lower stream systems couldn’t handle.
Most scholars who work in Southeast Asia attempt to establish the possible route through which early humans would migrate passing through the region after they migrated out of Africa. The evidence also indicates the migration route and settlement location along the routes that might have taken place during the Late Pleistocene and Early Holocene. There are three possible routes suggested by scholars; #From the northwest of Thailand they went down to Chao Phraya river basin and the Gulf of Thailand in which this route is supported by the faunal remains found in north Asia and Indonesia. Topographically advantages like the mountainous western flank of the Chao Phraya Basin, are likely to benefit the hominin habitats. Those advantages are “environmental mosaics with varied food resources and abundant water supplies, combined with physical features offering protection from the weather and providing tactical advantages in the pursuit of prey” #From Northeastern Vietnam they went down to the Indochinese region.
When originally built in the beginning of the 20th century, the Ottomans had the advantage of constructing the railway in what was then a relatively sparsely-populated area and as such had the benefit of being able to lay the railway on the most topographically convenient route between Haifa and Beit She'an. The renewed railway's route however had to contend with the significant population that settled in the area since, a complex set of existing infrastructure built up over the years, strict environmental considerations, and the wish to preserve as much open space as possible along the route. Therefore, the new route was in places considerably more difficult to construct and in some spots is also less direct than the original alignment. The modern railway splits from the Coastal Railway several kilometers east of the Haifa East Railway Station and curves to the north on its way towards Nesher atop one of the longest railway bridges in Israel, roughly paralleling Highway 75 and spanning over Highway 4 in the "Checkpost" area of east Haifa.
Western Thrace or West Thrace (, [Dytikí] Thráki / Turkish: Batı Trakya; , Zapadna Trakiya or Беломорска Тракия, Belomorska Trakiya) is a geographic and historical region of Greece, between the Nestos and Evros rivers in the northeast of the country; East Thrace, which lies east of the river Evros, forms the European part of Turkey, and the area to the north, in Bulgaria, is known as Northern Thrace. Inhabited since paleolithic times, it has been under the political, cultural and linguistic influence of the Greek world since the classical era; Greeks from the Aegean islands extensively colonized the region (especially the coastal part) and built prosperous cities such as Abdera (home of Democritus, the 5th-century B.C. philosopher who developed an atomic particle theory, and of Protagoras, a leading sophist) and Sale (near present- day Alexandroupoli). Under the Byzantine Empire, Western Thrace benefited from its position close to the imperial heartland and became a center of medieval Greek commerce and culture; later, under the Ottoman Empire, a number of Muslims settled there, marking the birth of the Muslim minority of Greece. Topographically, Thrace alternates between mountain-enclosed basins of varying size and deeply cut river valleys.

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